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Renseignements : POUR PLUS DE RENSEIGNEMENTS SUR VEUILLEZ VOUS ADRESSER À : la reproduction du contenu Services de publication du MDNM l'achat des publications du MDNM Vente de publications du MDNM les droits d'auteurs de la Couronne Imprimeur de la Reine PAR TÉLÉPHONE : Local : (705) 670-5691 Numéro sans frais : 1 888 415-9845, poste 5691 (au Canada et aux États-Unis) Local : (705) 670-5691 Numéro sans frais : 1 888 415-9845, poste 5691 (au Canada et aux États-Unis) Local : 416 326-2678 Numéro sans frais : 1 800 668-9938 (au Canada et aux États-Unis) PAR COURRIEL : [email protected] [email protected] [email protected] Industrial Mineral Background Paper #16 Barite and Fluorspar in Ontario: Resources and Options for Production By: Kilborn Limited and Mineral Development Section Ministry of Northern Development and Mines 1991 Ministry of Northern Development Ontario and Mines 1991 Queen's Printer for Ontario Printed in Ontario, Canada ISSN 0228-7811; 16 ISBN 0-7729-8583-9 Publications of the Ontario Ministry of Northern Develop ment and Mines are available from the following sources. Orders for publications should be accompanied by cheque or money order payable to the Treasurer of Ontario. Reports, maps and price lists (personal shopping or mail order): Public Information Centre, Ministry of Natural Resources Room 1640, Whitney Block, Queen's Park, Toronto, Ontario M7A 1W3 Reports and accompanying maps only (personal shopping): Publications Ontario Main Floor, 880 Bay Street Toronto, Ontario M7A 1N8 Reports and accompanying maps (mail order or telephone orders): Publications Services Section, Ministry of Government Services 5th Floor, 880 Bay Street Toronto, Ontario M7A 1N8 Telephone (local calls), 965-6015 Toll-free long distance, 1-800-268-7540 Toll free from area code 807, O-ZENITH-67200 Canadian Cataloguing in Publication Data Main entry under title: Barite and Fluorspar (Industrial mineral background paper, ISSN 0228-7811; 16) ISBN 0-7729-8583-9 Parts of this publication may be quoted if credit is given. It is recommended that reference to this report be made in the following form: Kilborn Limited and Mineral Development Section, Min istry of Northern Development and Mines 1991: Barite and Fluorspar in Ontario, Resources and Options for Pro duction; Ontario Ministry of Northern Development and Mines, Industrial Mineral Background Paper 16, 83p. Cover photo inset: Specimens of banded white barite from Hemlo and green fluorspar from Madoc, Ontario; barite and fluorspar are val ued industrial minerals in chemical manufacturing. Note: This paper does not represent official policy and the views expressed herein are not necessarily the viewpoint of the Government of Ontario. The authors represent that they have followed standard procedures in preparing the evalu ation in the Report, but the Report is based in part on details, information and assumptions provided by others and the authors, therefore, cannot guarantee the correctness of the Report; but to the extent of its investigation and within, the scope of the work delegated to it, the authors believe that the Report is substantially correct. Barite and Fluorspar in Ontario Table of Contents Summary .........................................5 1. General Introduction ...................9 Terms of Reference ..........................................9 Methodology....................................................9 2. Barite and Fluorspar Resources in Ontario...................................! l Introduction ...................................................11 Mineral Descriptions ......................................11 Previous Studies.............................................l3 History of Production.....................................14 Occurrences in Northwestern Ontario..............15 Occurrences in Northeastern Ontario...............22 Occurrences in Southeastern Ontario...............25 Commentary...................................................29 3. Options for Barite Mineral Production..................................31 Existing Production........................................31 Production Options.........................................31 Production Costs ............................................35 4. Options for Barium Chemicals Production..................................41 Production Options.........................................41 Production Costs ............................................57 5. Options for Fluorspar Production..................................61 Production Options.........................................61 Specifications ................................................62 Production Costs ............................................64 6. Implications for Small Mines ......65 Custom Milling ..............................................65 By-Product Recovery .....................................66 7. Conclusions and Recommendations.....................69 Conclusions ...................................................69 Recommendations ..........................................70 Selected Bibliography ...................71 Resources ......................................................71 Options for Production ...................................73 Appendices....................................... A. B. C. Barite Mill Processing Equipment ...........75 Major Items and Typical Costs...........76 Barium Chemicals Plant Equipment.........77 Major Items and Typical Costs...........78 Fluorspar Mill Processing Equipment Major Items and Typical Costs...........81 Barite and Fluorspar in Ontario Summary The prime objective of the study was to evaluate the technical and economic potential of barium chemicals and high quality fluorspar (fluorite) in Ontario based on small mining operations, by-product mineral recov ery, custom mineral processing and established/ emerging chemicals production technologies. There are numerous recorded occurrences of barite and/or fluorspar throughout Ontario. Up to 1961, the province was a producer of fluorspar from shallow workings in vein deposits in Southeastern Ontario; barite has been extracted from several veins, principally in Northern Ontario, for periods dating back to the last century. Further exploration of these occurrences, to investigate the possibilities of economic reserves, have rarely been carried out. The present-day viability of working small deposits for specialty markets has been successfully demonstrated by the province's current producer of barite in Northeastern Ontario. Metals exploration programs in recent years have led to the incidental discovery of significant deposits of these industrial minerals in terms of volume, for example, that of stratiform barite in the Hemlo gold belt, and of fluorspar in the SpringpoleLake alkalic igneous complex, both in Northern Ontario. Such dis coveries encourage the view that concentrations of potential interest remain to be identified by explorationists in the province. Barite A review of barite mineral resources in the province of Ontario revealed that mineral deposits of Northern Ontario in the Thunder Bay area and the Matachewan area or by-product barite contained in gold mill tailings from Hemlo area mining operations could potentially support the production of 15,000 to 30,000 tonnes per year of high grade barite (94*2fc BaSO4, minimum). A central processing mill treating ore from one or more mining locations would be required in order to produce 30,000 tonnes per year of barite in either mineral deposit area (Thunder Bay or Matachewan), whereas, a single processing mill could produce the required tonnage of barite from a portion of the Hemlo area gold mill tailings. Capital requirements and total production costs for the production of barite depend on the location of the processing mill or mills, the quantity of barite being produced and the grade of the barite ore/gold mill tail ings material and are shown in Table l. The total production costs include all direct oper ating costs, capital recovery charges and product shipping charges to a barium chemicals plant in the Thunder Bay area (for the Thunder Bay and Hemlo mill locations) or in a central Ontario location closer Summary Table l Capital Requirements and Productions Costs for Various Mill Locations Mill Capacity, Capital Cost Total Production Cost, Mill Location t/a S S/t Barite Thunder Bay 30,000 15,000 3,000,000 3,000,000 108 151 Matachewan 30,000 15,000 3,000,000 3,000,000 213 274 Hemlo 30,000 8,400,000 180 to the barium chemicals markets (for the Matachewan and twin mill locations). The indicated price of S108 per tonne for 30,000 tonnes per year of barite from a single Thunder Bay mill is considered to be optimistic as established barite reserves in the area may not be sufficient to support the 30,000 tonnes per year operation. A more realis tic price to consider for 30,000 tonnes per year of barite is 5180 to S210 per tonne, based either on the recovery of barite from Hemlo area gold mill tailings or on its production in twin 15,000 tonnes per year mills in the Thunder Bay and Matachewan areas, with barite being shipped to a centrally located chemicals plant. All costs developed in this study must be con sidered preliminary as they are based on a minimum level of information concerning mineral deposits, met allurgical testing and processing options. Employment opportunities would be created with the introduction of a new barite mining and milling oper ation in Ontario. The number of jobs created depends on the barite mill location, the mill capacity and the type of operation and are shown in Table 2. Additional job opportunities would be created in the Thunder Bay and Matachewan cases for contract mining of the barite ore. Barium Chemicals An investigation of potential market opportunities for barium chemicals resulted in an evaluation of the technical and economic potential of producing barium sulphide (BaS), barium carbonate(BaCO3), barium chloride (BaCh), barium sulphate (BaSCU), barium oxide (BaO) and barium hydroxide (Ba(OH)2) in an integrated chemicals complex capable of processing 30,000 tonnes per year of barite: * BaS 20,000 tonnes per year, primarily for cap tive use but with up to 4,400 tonnes per year available for sale * BaCOs 16,000 tonnes per year capacity, with normal production rates of 12,000 tonnes per year for sale and l ,950 tonnes per year for captive use (BaO production) * BaCh 5,000 tonnes per year capacity, with a normal operating rate of 3,500 tonnes per year * BaSO4 l ,500 tonnes per year capacity, with a normal production rate of l ,000 tonnes per year. Table 2 Job Creation for Various Mill Locations Mill Capacity, Mill Location t/a Estimated Job Creation Thunder Bay 30,000 15,000 14 11 Matachewan 30,000 15,000 15 30,000 17 Hemlo 12 Barite and Fluorspar in Ontario Table 3 Capital and Production Costs for Various Barium Chemicals Plant Gate Production Cost, S/tonne Capital Cost, Barite @ Barite @ Chemical S million SlOS/t Sl80-2107t BaS BaCOa BaCI 2 BaSO4 BaO Ba(OH) 2 Monohydrate Octahydrate 11 7 4.8 1.6 4.6 413 592 1098 1085 1890 520-565 685-725 1185-1220 1165-1200 2010-2060 - 1535 920 1635-1675 980-1000 Capital Cost Total Facility 29 * BaO and Ba(OH)2 3,000 tonnes per year BaO capacity, with a normal operating rate of 1,500 tonnes per year BaO equivalent, as barium oxide and hydroxides. The precursor of most barium chemicals is BaS including, BaCOs, BaCh, and BaSO4. Barium car bonate is used as the raw material in the production of BaO7Ba(OH)2. Capital costs and plant gate production costs for the barium chemicals depend on the chemical being produced, the cost of raw materials and the plant capac ity illustrated in Table 3. Sodium sulphide (Na2S) is produced as a by-prod uct during the production of BaCOa, BaCh and BaSO4. It is recovered for sale to the pulp and paper industry as a substitute for NaiSO4 in Kraft pulp mills. Based on an analysis of reported market prices for barium chemicals (Law, Sigurdson and Associates, SRI Inter national 1989), it appears that the production of barium sulphide, barium carbonate and, possibly, barium sul phate offers reasonable technical and economic potential provided that low-cost barite can be delivered to the barium chemicals plant and that their reported market prices are realistic for large quantity sales (Table 4). The above cost for BaSO4 is based on its production in a multi-product plant capable of producing BaCOs and BaSO4 in blocked operation. Earlier costs, S l,085 to S l,200 per tonne, were based on production in a dedicated process unit. The production of BaCh, BaO and Ba(OHh does not appear to have any significant economic poten tial as indicated production costs. (Table 5) are well in excess of reported market values. Employment opportunities would be created with the production of barium chemicals in Ontario. An esti mated operations, maintenance and administration staff of 38 personnel would be required for a barium Table 4 Production Costs and Market Value for some Barium Chemicals Estimated Production Reported Market Chemical Cost, S/tonneValue, S/tonne BaS 413-565 N/A BaCI2 592-725 550-800 BaSCU 815-930 800 Summary Table 5 Production Cost and Market Value for Barium Chemicals Estimated Production Chemical Cost, S/tonne Reported Market Value, S/tonne BaCI 2 BaO 1098-1220 1890-2060 500-840 N/A Ba(OH) 2 Monohydrate Octahydrate 1535-1675 920-1000 1100-1200 N/A chemicals plant capable of producing BaS, BaCOs and BaSO4. Additional staff would be required to market the barium chemicals in Canada and the Eastern Unit ed States. Fluorspar A review of fluorspar reserves in the Madoc area of South-Eastern Ontario indicated that local mineral deposits could possibly support the production of 15,000 tonnes per year of acid grade fluorspar (97*36 CaFz, minimum) or 20,000 tonnes per year of metal lurgical grade fluorspar (709fc CaFi). Capital requirements and total production costs for the production of fluorspar depend on the mill location, the ore grade and the quantity and grade of fluorspar being produced (See Table 6). Low shipping costs for these materials to Ontariobased consumers should overcome the probable lower production costs of major suppliers of imported material, making the Ontario-produced product econo mically attractive. Total imports into Canada amounted to 194,000 tonnes of all grades in 1988, thus the iden tified market potential. Employment opportunities would be created with the introduction of a fluorspar mining and milling opera tion in Ontario. An estimated staff of 14 personnel would be required for the fluorspar milling operation, plus additional contract mining jobs. Recommendations Before serious consideration can be given to the development of barite and fluorspar reserves in Ontario and the production of barium chemicals (to take advan tage of potential market opportunities in Canada and the Eastern United States) additional work should be undertaken to establish the reliability of the most attractive options. 1. Base level proven and probable reserves should be established. 2. Representative ore samples should be tested to develop cost effective metallurgical process ing routes. Potential mine and processing mill locations should be examined and feasibility studies should be conducted to assess select ed mineral processing options and costs. 3. Market opportunities for barium chemicals should be clearly defined, potential chemical plant locations should be examined and a detailed feasibility study should be complet ed to assess selected barium chemicals production options and costs. Table 6 Capital requirements and production costs for acid and metallurgical grade fluorspar Total Fluorspar Mill Capacity, Capital Cost, Production Cost, t/a S/tonne Grade S Acid 15,000 3,800,000 198 Metallurgical 20,000 2,000,000 90 Barite and Fluorspar in Ontario 1.General Introduction This study was commissioned by the Mineral Devel opment and Lands Branch of the Ontario Ministry of Northern Development and Mines as an extension of a study previously completed for the Ministry by Law, Sigurdson and Associates and SRI International (1989). The earlier study identified chemical derivatives of barite and fluorspar as two of the potential commer cial opportunities in Ontario on the basis of market opportunity, mineral resource potential and existing industrial service infrastructure. This document is based on a study report received in March 1990 from Kilborn Limited. The second chapter Barite and Fluorspar Resources in Ontario is a literature review by the Mineral Development Section of the Ministry of Northern Development and Mines and is an edited version of an internal report by D.M. Conrod of the Section. Funding was provided by the Economic Develop ment Program of the Canada-Ontario 1985 Mineral Development Agreement (COMDA). COMDA was a subsidiary agreement to the Economic and Regional Development Agreement (ERDA) signed by the Gov ernments of Ontario and Canada in 1984. Terms of Reference The principal objective of the study was to evalu ate the technical and economic potential for the production of barium chemicals and high quality fluorspar in Ontario based on small mining opera tions, by-product mineral recovery, custom mineral processing and existing or emerging chemicals pro duction technologies. Barite and fluorspar mineral supply options were to consider resource development in Northern and Eastern Ontario, by-product mineral recovery and mineral processing required to produce high quality barite (94^o BaSO4) and metallurgical grade or acid grade fluorspar (6096 and 979fc CaF2, respectively). Barium chemical production options were to include BaS, the precursor of most barium chemicals; a number of the high demand derivatives, BaCOs and BaCh; and additional secondary deriva tives, BaSO4, BaO, barium peroxide (BaOz), barium hydroxide (Ba(OH)2), barium nitrate (Ba(NOz)2) etc. Methodology The initial activity in the study was the collection and review of available information on barite and fluorspar mineral resources in Ontario, mineral recov ery techniques and barium chemical production methods and costs. The major activities in completing the study were: Introduction 1.Review of barite and fluorspar mineral resources in Ontario, by-product barite or fluorspar recovery possibilities. 2. Evaluation and selection of potential recovery methods for barite and fluorspar minerals, development of preliminary production costs. 3. Selection of barium chemicals to be studied. 4. Evaluation and selection of production meth ods for barium chemicals, development of preliminary production costs. Barite and fluorspar mineral resources in Ontario were reviewed in order to determine the potential for commercial production at rates in the range of 30,000 tonnes per year barite (to support a commercial scale barium chemicals operation) and 10,000 to 15,000 tonnes per year of metallurgical grade or acid grade fluorspar. Consideration was given to the develop ment of mineral resources, the recovery of by-product barite from gold mill tailings, the potential joint recov ery of barite and fluorspar, the development of a number of small mineral deposits to meet the target production rates and the possible expansion of exist ing barite production facilities. Based on the results of the resource review, pro cessing steps required to recover high quality barite and acid grade or metallurgical grade fluorspar from open pit or underground mining operations and gold mill tailings were assessed and appropriate processing schemes were developed. This was followed by the development of preliminary capital cost and produc tion cost estimates for each recovery option. In all cases that involved the processing of mineral reserves, the concept of an area processing plant being supplied with barite or fluorspar ore from several small mines in the vicinity of the plant was considered. Production costs for the alternative processing schemes were compared and the processing routes showing the greatest economic potential were select ed. High quality barite was considered as the raw material for the manufacture of a variety of barium chemicals, whereas, fluorspar (acid grade or metal lurgical grade) was assessed on the basis of competitive sales in Ontario, other regions of Canada and the East ern United States. Potential opportunities for marketing barium chem icals in Canada and the Eastern United States were reviewed in order to select the barium chemicals included in the study, consisting of barium sulphide, the high demand derivatives barium carbonate and barium chloride, and additional secondary derivatives. This was followed by a review and selection of pro duction alternatives for the barium chemicals, including established and emerging technologies and 10 processes that co-produced valuable by-product chem icals. The possibility of producing multiple chemicals in a single production facility in blocked operation was considered, particularly for the lower demand derivatives. Simplified flow plans and overall material balances were developed for the production of commercial quan tities of the selected barium chemicals, based on processing 30,000 tonnes per year of high quality barite (949fc BaSO-O from a Northern or Eastern Ontario ore processing plant. Preliminary capital cost and pro duction cost estimates were developed for each barium chemical, taking into account appropriate credits for the sale of by-product chemicals. Blocked operation for the production of multiple chemicals in a single facil ity was evaluated, where practical, in order to lower the production costs of low demand secondary chemicals. Production costs were compared to current market prices for the individual barium chemicals to determine their economic potential. Marketing of barium chem icals in Canada and the Eastern United States is considered to be a potential commercial opportunity as there is no Canadian production and only limited U.S. production. In this study report, all costs are expressed in 1990 Canadian dollars. All tonnage values are metric tonnes unless otherwise noted. Additionally, fluorspar is used to describe the mineral fluorite as well as the metal lurgical grade or acid grade product fluorspar. Barite and Fluorspar in Ontario 2. Barite and Fluorspar Resources in Ontario Introduction Ontario, currently, has one small producer of barite. The province is a past producer of fluorspar; mining was discontinued in 1961. The geological literature records over 300 occur rences of barite and/or fluorspar throughout the province, ranging from showings of interest only to the collector through to deposits of significant potential tonnage, such as those of the Hemlo area (barite) and the Red Lake area (fluorspar) in Northern Ontario. Most of the occurrences are narrow veins or fine dis seminations within a variety of host rocks of various geological ages. While the majority of the veins are small and often discontinuous, many are of good insitu grade. Fluorspar and barite are often found together, with many of the occurrences in Ontario being concentrat ed in local areas; for example, 71 occurrences are located along two zones in the Thunder Bay area, 46 occurrences are reports in the Madoc-Moira Lake area and 28 occurrences are noted in the contiguous town ships of Cardiff and Monmouth. The only known stratiform barite deposit in Ontario is found in the gold ore zone of the Hemlo belt in Northern Ontario, and it also represents the largest barite occurrence in the province. The summary of mineral resources in the following pages includes brief descriptions of selected principal occurrences. Map l is an index to the location maps for regions and districts of Ontario with occurrences of barite and fluorspar. Further details on specific occurrences in the province can be obtained from the references cited at the end of Part One and also by referring to the appropriate files in the offices of the Resident Geologists of the Ministry of Northern Devel opment and Mines. Mineral Descriptions Fluorspar Fluorspar (CaF2), also known as fluorite, fluor, Blue John or Derbyshire spar, is the principal ore of fluo rine. Fluorspar is used as a flux, in the manufacture of hydrofluoric acid, in the preparation of glass and enam els and for carved ornaments. Fluorspar is a transparent to translucent mineral that crystallizes in either fine-grained aggregates or as coarse, individual crystals. Pure fluorspar consists of Sl.33% calcium and 48.669k fluorine by weight. Deer et al. (1980), state that most natural fluorspar is at least 999fc CaFi, with Barite and Fluorspar Resources in Ontario 11 MAP 1. Index to Location Maps of Barite and Fluorspar Occurrences in Ontario. 12 Barite and Fluorspar in Ontario minor amounts of silicon, aluminium and magnesium as impurities or inclusions within the fluorspar struc ture. Strontium, yttrium and the rare earth elements may replace a small portion of the calcium in fluorspar. Fluorspar is a relatively soft mineral, having a hard ness of four on the Mohs' scale. The refractive index of fluorspar varies between 1.433 and 1.435. The spe cific gravity of fluorspar ranges from 3.0 to 3.6 in massive finely crystalline varieties, while individual coarse crystals have a specific gravity of 3.2. Fluorescence, a phenomenon which derives its name from fluorspar, is often strong and has been correlat ed to high contents of the rare-earths lanthanum, europium and cesium, (Deer et al. 1980). Yttrium and samarium may also play a role in the fluorescence of green fluorspar. Natural fluorspar occurs in a wide range of colours. The presence of impurities within the crystal lattice, including the rare-earth elements (REEs), oxygen, hydrogen, water vapour, as well as the presence of colloidal particles, variations in the growth rate of the crystals, variations in pressure during and after crys tal formation and exposure to light all contribute to the colour of fluorspar. (Naldrett et al. 1987) Although the intensity of coloration increases with an increase in the REE content, there is no apparent association between the presence of a particular REE and the colour of the fluorspar. Barite Barite (BaSO-O, also termed barytes, heavy spar or cawk, is the principal ore of barium. It is chiefly used in drilling muds and is an important ingredient in paint, paper and textile manufacture. Barite is colourless or white and displays a vitreous to resinous lustre. The presence of impurities, includ ing iron oxides and hydroxides, sulphides, and organic matter give barite a yellow, red or brown colour. Pure barite contains 58.84 weight 9fc barium. Most barite is pure BaSO4; however, barium can be replaced by strontium in a continuous solid solution series from barite to celestite (SrSO4). Lead and calcium can occa sionally replace barium within the crystal structure (Deer et al. 1980). The high specific gravity of approx imately 4.5 is a feature of the mineral; this increases or decreases with the substitution of lead or strontium respectively for barium. Natural barite is usually found as well-formed tabu lar crystals in the orthorhombic system or as fine-grained aggregates occurring in globular, fibrous, lamellar or granular arrangements. Platy crystals, arranged in clus ters, are often given the name of "desert rose." Barite and Fluorspar Resources in Ontario The hardness of barite ranges between 2.5 and 3.5 on the Mohs' scale. Previous Studies A number of papers concerning Ontario fluorspar and its products were published between the early 1940's and early 1960's, corresponding to the rela tively high production of fluorspar during that period. Guillet (1963) provided a detailed historical and geo logical compilation of barite occurrences in Ontario. The same author also published detailed historical and geological data for fluorspar in the Madoc-Moira Lake area (Guillet 1964). A program of drilling, bulk sampling and benefi ciation tests was carried out between 1941 and 1951 by the Geological Survey of Canada to evaluate the Madoc area's fluorspar resources at the former fluorspar-producing properties. Drilling results are summarized in Guillet (1964). Detailed mineralogical and petrological studies of the Madoc ores were undertaken by Rupert (1963) and Mielke (1977). Rupert, through fluid inclusion anal yses, determined that the ores were precipitated from several generations of solutions, ranging in tempera ture from 103 0 to 148 0C. Mielke concluded that at least seven periods of fault activity and associated low temperature and low pressure hydrothermal min eralization can be recognized in the Rogers mine. Two sulphosalts, boulangerite and semseyite, were recog nized with galena in the ore. Mielke concludes that these minerals grew from relatively cool dilute alkalirich solutions. Lalonde (1974) undertook a geochemical study of the secondary dispersion of fluorine in the MadocMoira Lake area, and concluded that most of the rocks within the area are enriched in fluorine. The fluorine content of groundwater was found to delineate areas of known fluorspar concentration. A number of geophysical surveys were undertaken in the immediate Moira Lake area by Thompson and Williams between the years 1985 and 1990. These studies involved seismic, magnetic, resistivity, radio activity and alpha meter surveys along six transects in an attempt to locate unknown faults and the exten sions of known faults which may contain vein material. Thompson and Williams (1989) have recently com bined their geophysical and structural studies of the area with the results of Lalonde's 1974 geochemical survey to locate potential ore targets. High concen trations of fluorine tend to fall along known or inferred faults in the area or at fault junctions. A recent detailed mapping and geochemical soil 13 survey was undertaken in the Moira Lake area by Der ry, Michener, Booth and Wahl in 1989 (Dickson and Trinder 1989). The survey resulted in the recognition of several coincident fluorite-barite-zinc target anomalies. Summary compilations of fluorspar and barite occurrences in Ontario are provided by Vos et al. (1983) for Northern Ontario and Martin (1983) for the Algonquin Region. Several studies of the barite located in the Hemlo area have been undertaken during the last six years. Roach (1987) carried out a petrological study of the Western Barite Occurrences located approximately 25 km west of Hemlo. He concluded that the occur rences were located in zones of heterogeneous ductile shear and that the barite-sulfide mineralization occurred before or during the ductile shearing event. Gliddon (1985) undertook a petrological study of the barite at Hemlo, concluding that the deposit is most likely syngenetic in origin. Later studies of the deposit by Valliant and Bradbrook (1986) and Walford et al. (1986), however, suggest that the deposit may be epi genetic in origin. The question of origin is still to be settled. Fluorspar and barite mineral collecting sites in Ontario are documented in a series of publications by Sabina(1963, 1969, 1971, 1976, 1983, 1986, 1987). Petrological research and mapping to date of the Springpole Lake alkalic carbonatite complex and its associated fluorspar mineralization has been reported by Barron et al. (1989). In addition to these studies, information concerning specific properties are available in the Ministry of Northern Development and Mines Assessment Files. History of Production Fluorspar Between 1905 and 1961, 121,919 tons of fluorspar, mostly of metallurgical grade, were shipped from mines in the southeastern part of the province. Much of this production was achieved in response to wartime demand, as shown in Table 7. The dominant fluorspar-producing area in Ontario has been in the Madoc area, where over 30 workings were recorded. Five properties, Rogers, Bailey, Noyes, Kilpatrick and Perry mines, accounted for 939fc of Ontario's recorded shipments. The principal produc er was the Rogers mine, which yielded a total of 45,000 tons, including 40,000 tons within a nine-year period. Only 129 tons of fluorspar shipments were record ed from Cardiff Township from the Dwyer, Clarke and 14 Table 7 Fluorspar Production in Ontario (Modified after Guillet 1964) Period Shipments (tons) 1905-1911 1916-1920 1921-1939 1940-1951 1952-1961 44 19,936 1,754 86,543 13,642 Tripp mines. There has been no fluorspar production in Ontario since 1961. Mining in the Madoc area was carried out by small independent operators and only the pure, easily-sort ed fluorspar was recovered. There was no mill for separation of the fluorspar in the banded calcite-baritefluorspar portions of the veins. The mine-run ore was usually crushed and run over a picking belt where most of the lump fluorspar was recovered. This highgrade material was diluted with some of the calcite-fluorite-barite fines to ship 7096 CaFz metal lurgical grade. Mining was limited to shallow depths (110 m or less) because of heavy water flows, which the small mines did not have the equipment to control. When fluorspar production ceased in the Madoc area, an undetermined amount of ore remained at the bottom of the Rogers, Kilpatrick, Perry Lake, Perry and Blakely mines, with vein widths reported of between 1.0 and 1.6 m. Barite Between 1885 and 1948, 9,899 tons of barite were shipped from Ontario operations. This ore was extract ed by surface mining of high-grade veins by manual methods, including hand-cobbing, at McKellar Island (Thunder Bay area), Langmuir Township and Penhor wood Township in northern Ontario and in North Burgess Township in the southeastern part of the province. There is only one current producer of barite in the province. Extender Minerals of Canada Ltd. began operations in 1967 and has produced approximately 200,000 tons of barite since that date from a number of veins in the Matachewan area of northeastern Ontario. Ore is extracted from four sub-parallel veins in Yarrow Township, one vein in Penhorwood Town ship and one vein in Cairo Township. Production from a vein deposit in North Williams Township, in the Shining Tree Area, is expected to commence in 1991. Barite and Fluorspar in Ontario After originally being worked from surface, the veins are now mined by Extender Minerals by under ground methods, producing a total of approximately 25,000 short tons of ore per annum grading 50 to 609fc BaSO4 prior to treatment. The barite ore is partially upgraded at the mines sites and then trucked to a treat ment plant in Matachewan. The ore is dried and finely ground to -45 jim at the plant; the product, grading 93 to 979k BaSCU, is bagged for sale in mineral filler markets. Table 8 summarizes barite production in Ontario to the present day. Table 8 Barite Production in Ontario (Modified after Guillet, 1963) Period Shipments (tons) 1885-1887 1888-1890 1892 1894 1918-1948 1976-present 4,564 2,942 315 1,081 995 200,000 est. Occurrences in Northwestern Ontario Barite and fluorspar occurrences are concentrated along two fault zones west of Thunder Bay and along the Archean-Proterozoic unconformity in the Dorion area. Another concentration of barite veins is found in the Mazokama Bay area near Nipigon. The most sig nificant known deposit of barite, in terms of tonnage, is the stratiform occurrence in the Hemlo Belt east of Marathon. Fluorspar locations are documented near Rossport, Lake of the Woods, Sturgeon Lake (northeast of Ignace) and also in association with quartz-molyb denite veins at other properties. The largest occurrence of fluorspar to date is reported within the Springpole Lake carbonatite near Red Lake. The occurrences in Northwestern Ontario are shown in Map 2. Thunder Bay Dorion Area Barite/Minor Fluorspar Calcite and barite are the major constituents of two parallel, northeasterly-trending zones in the Thunder Bay Area. The presence of fluorspar appears to be largely restricted to the northern system. The veins of both zones contain minor amounts of silver that was recovered in the latter part of the 18th century. The Dorion area is characterized by a number of lead and zinc-bearing barite veins of similar orientation to that of the northern vein-fault system of the Thunder Bay area. Occurrences in the Thunder Bay and Dorion areas are located in Map 3. Northern Vein System: Thunder Bay Area The northern vein system trends 067 0 and is gen erally vertically-oriented. It has, however, been documented to dip steeply to the north in some loca tions and steeply to the south in others. The veins occupy faults that cut the Logan diabase sills and mid dle Precambrian sedimentary rocks of the area. The being material consists of calcite, quartz, fluorspar, barite, minor disseminated sulphides (including pyrite, galena, sphalerite and chalcopyrite), as well as native silver and argentite. The vein material acts as a frac ture in-fill, cementing pieces of the country rock within the fault zone. Although most of the individual veins and faults that comprise the system are approximately l m wide, some veins such as those located on the Rabbit Moun- Barite and Fluorspar Resources in Ontario 15 g 6 •4— 6c -2 V) (D Vi (D O C 0) o o O b a t/) o o LJ- •D C. o o b CO 16 Barite and Fluorspar in Ontario Barite and Fluorspar Resources in Ontario 17 tain, Neepatyre, and the Paresseux Rapids properties are up to 6 m wide. Calcite within the veins is usually coarsely crys talline and white or occasionally pink in colour. The green and purple varieties of fluorspar occur individ ually or inter-banded within the veins. Yellow fluorspar is less common, but is reported to occur at the past-pro ducing Federal Mine. Often the fluorspar surrounds calcite in a colloform texture. Quartz is ubiquitous in the veins that comprise the system occurring in trans parent, white, smoky, amethyst, and rose varieties. The barite is generally white and coarsely crystalline. Sulphides are disseminated throughout the vein material. Native silver occurs in fern-like and wire forms, while argentite occurs as films, sheets, and sol id nuggets up to several ounces in weight. Recent trenching and drilling has been undertaken in O'Connor Township on the McDermott-Cox barite showing (mining location: T144). The vein-fault zone can be traced on surface for approximately 450 m, and varies in width from 1.5 to 9 m. The vein consists of barite, calcite, amethyst, white quartz and fluorspar, with minor amounts of galena sphalerite. Barite com prises 20 to 609fc of the vein material, while calcite accounts for between 10 and 209fc and quartz accounts for between 30 and 409fc. At the McDermott-Cox show ing, the vein dips steeply to the north; however, on the adjoining property, mining location T143, the vein is reported to dip between 500 and 75 0 southeast (Tan ton 1931). The vein is exposed over a length of 46m with an average width of 1.5 m on the adjacent T143 proper ty. Tanton (1931), reports that the vein consists of coarsely crystalline, platy barite, white calcite, and quartz, with small amounts of green fluorspar and minor disseminated galena. Barite accounts for approx imately one-third of the vein material and occurs in close spatial association to the calcite. At both the McDermott-Cox and T143 properties, the host rock is Animikie banded and oolitic iron formation, shale, and volcanic lapilli and ash tuff (Tanton 1931). The pinching and swelling of the vein and the varying pro portions of vein minerals along strike make estimates of tonnage and grades difficult. The largest vein widths recorded in the area are located on the Silver Mountain, Rabbit Mountain, Neepatyre, Paresseux Rapids, Federal, Silver Falls, Woodside and Star properties. These are scattered along the strike of the northern zone and are probably a reflection of the "pinch-and-swell" nature of the vein system. 18 Southern Vein System: Thunder Bay Area There are sixteen barite occurrences that comprise the southern zone and are hosted within the verticallyoriented, north-easterly-trending Pine River-Mount Mollic gabbroic intrusion. This intrusion contains two sets of vertically-oriented joints, one trending 135 0 and the other trending 800 . Almost all of the calcitebarite veins that comprise this system strike 315 0 and are either vertically-oriented or dip moderately to the northeast. The veins most likely occupy pre-existing joint fractures. The veins of this southern zone vary from l m to over 20 m in thickness and consist predominantly of calcite and barite, with minor amounts of amethyst, fluorspar, pyrite, chalcopyrite, galena, sphalerite, cobaltite, smaltite, tetrahedrite, silver and argentite. The grades of the veins vary substantially over short distances, but are generally high, between 84 and 9096 BaSO4 where documented. The Jarvis Island vein strikes 135 0 and dips 40 0 to 60 0 to the northeast. Widths vary from 4.5 to 2 m over a distance of 244 m. At the southeastern end of the vein, it consists of approximately 809fc calcite, 109fc barite and 1096 quartz. The northwestern end of the vein consists of approx imately 509fc barite. Minor amounts of fluorspar are recorded on the property. In the case of McKellar Island, the barite vein also strikes 135 0 but is verticaloriented. Widths of the vein vary from 9 to 21 m over a strike length of 110 m. The vein material consists of approximately 509fc barite with lesser amounts of cal cite and quartz. Dorion Area Tanton (1931) documented thirty separate leadzinc-barite occurrences with the Dorion area. These occurrences consist of mineralogically-zoned, lead and zinc-bearing, calcite-quartz-barite veins, located along the unconformity separating the Archean Quetico gneiss belt and Middle Precambrian metasedimentary rocks of the Gunflint and Rove formations from the late Precambrian sedimentary rocks of the Sibley Group. The veins are characterized by a galena-calcite core, a sphalerite-quartz central zone, and a barite zone in the vein extremities along strike. The veins are similar in orientation and width to those of the north ern vein-fault system in the Thunder Bay area. Franklin and Mitchell (1977) claimed that these occurrences constitute a distinct metallogenic entity, confined to the Sibley Group redbed basin, and that they are clearly distinguishable from the occurrences that constitute the northern Thunder Bay vein-fault system. Barite and Fluorspar in Ontario Of the thirty occurrences, only the Dorion, Enter prise and Ogema deposits were mined in the past for their lead and zinc contents. The veins typically con sist of quartz, calcite and barite with minor fluorspar at these mines. The principal sulphide minerals are galena, sphalerite, pyrite, marcasite, chalcopyrite and chalcocite. The vein system at the Dorion deposit comprises five separate veins extending for approximately 1525 m. The largest single vein is 2.4 m wide and extends along strike for 244 m. The barite occurs in the central portion of some veins and as distinct veinlets cross-cutting other portions of the vein system. Tan ton (1931) reports one 1.3 m wide vein containing 209fc sphalerite. Brecciated fragments of the wallrock can account for between 209fc and 80*?fc of the vein. The Enterprise Mine is hosted within the Sibley Group sedimentary rocks. The vein system trends 065 to 075 0 , parallel to the Sibley Group-Archean unconformity. The 15m wide system consists of approximately 10 cm wide veins, which occupy ver tical joints within the Rossport formation. Fragments of wallrock account for less than 209b of the vein material. The Ogema Mine is hosted within the Archean metasedimentary gneisses and pegmatites and con tains veins that range from 2 to 5 cm in width. Red Lake Area Fluorspar The Springpole Lake property is located approxi mately 110 km northeast of Red Lake, within the Birch Lake Greenstone Belt, and geologically represents a small alkaline volcanic centre. Both extrusive and intrusive rock types, including fluorite-bearing, sovitetype carbonatite bodies, comprise what is referred to as the Springpole Alkalic Volcanic Complex (Barron et al. 1989). Flows and pyroclastic deposits of the complex unconformably overlie the older Archean metavolcanic rocks of the area, and the complex is overlain by Temiskaming-type metasedimentary rocks. Porphyritic syenite and trachyte are the most abundant lithologies of the complex. The fluorspar-bearing carbonatite intrusion accounts for only a small portion of the complex. It is exposed on surface at two locations but Barron et al. (1989) report a strike length of at least 1.5 km. The carbon atite is in sharp contrast with the surrounding, fenitized, country-rock breccias. Fluorspar occurs as fine disseminations and stringer veinlets within the carbonatite and adjacent fenitized breccias. In addition to calcite and fluorite, the carbonatite may also con tain up to several percent barite and quartz. In the Barite and Fluorspar Resources in Ontario exposed portion of the carbonatite, fluorspar averages 10 to 15 volume 9fc of the rock. The property is currently being investigated by Noranda Limited and Akiko-Lori Gold Resources Ltd., gold is the main mineral of interest. Recent diamond drilling on the property was reported to have inter sected significant amounts of fluorspar in several holes, including one intersection of 32 m (drill width) averaging 27. 99fc Sturgeon Lake Area Fluorspar The Sturgeon Lake area is located 76 km east of Sioux Lookout, within the Wabigoon Subprovince of the Canadian Shield. Within the immediate Sturgeon Lake area, Trowell (1983) has identified three alkalic complexes and proposes that all three are coeval and comagmatic. The Wahl and Texmont properties are located with the Sturgeon Narrows Complex. Fluorspar occurs as fine disseminations throughout all rock types of the complex, accounting for up to 19fc of the rock. Local concentrations of fluorspar are reported to occur along a sheared carbonatized zone on Sturgeon Narrows Island (Trowell 1983). Diamond drilling on the Wahl property by W.G. Wahl Limited in 1969 intersected fluorspar mineralization along with minor strontianite and vanadium mica. Diamond drilling by Selco Explo ration Company Limited in 1970 did not locate any significant concentrations of fluorspar. Recent dia mond drilling by Primrose Gold Resources in the area in 1989 also has not intersected significant concen trations of fluorspar. Trowell (1983) documented concentrations of fluorspar reaching a few percent in volume occurring along joints in the rocks located along the south shore of East Bay. Although the Squaw and Bell Lake Complexes are similar to the Sturgeon Narrows Complex, Trowell has not reported the presence of fluorspar or carbon ate (possibly carbonatite) zones in these two complexes. Lake of the Woods Area Fluorspar Fluorspar on the Thrasher Property occurs within a quartz-carbonate vein system, 1.3 m in width, that cuts felsic and lapilli tuff; the deep purple fluorspar forms fine-grained veinlets. The vein contains up to 159fc fluorspar over short distances; the best intersec tions obtained in diamond-drilling, undertaken in 1964, reported visual estimates of 10*?fc to 309fc fluorspar over 3.5 m. A geophysical survey, undertaken by Esso Miner als Canada in 1984, indicated that the fluorspar-bearing core of the Lobstick Bay shear zone cannot be traced 19 by geophysical techniques, and that the gold-bearing zone does not outcrop along strike to the east or west of the main zone (MNDM Assessment Files). Nipigon-Schreiber Area Barite/Fluorspar The Halonen-Cavers Hill fluorspar-barite property is underlain by an igneous complex composed pre dominantly of potassic feldspar-rich granite and granodiorite, cut by quartz-feldspar pegmatite veins and pods. In addition to the purple fluorspar coating joint sur faces of the complex, three fluorspar-barite quartz veins occupy an easterly-trending breccia zone. Vein widths range from 1.3 to 18 m (Brown 1973). The results of a reconnaissance mapping and water and stream sediment sampling program, undertaken by Asarco in 1973 (Brown 1973), indicate that the mineralized breccia zone has a series of isolated fluorspar showings covering a strike length of 915 m. Sampling of the vein over widths of 3 m range between l and 109fc fluorspar with one sample yielding 23.11*70 CaF2 over 3m. The results of the geochemical survey did not reveal any new fluorspar showings. Drilling by E. Former in the area in 1982 and 1987 did not reveal any new fluorspar occurrences. Three mineralized zones occur at the Pays Plat fluorspar occurrence informally known as the Chishol Pit Zone, the Main Adit Zone and the Northern Creek Zone. The Chishol Pit Zone consists of a one metre wide quartz-calcite-fluorspar vein that occupies a steeplydipping breccia zone trending 1700 through Archean granite. The vein contains pyrite, galena and spha lerite as local sulphide-rich seams. At the Main Adit Zone, a quartz-fluorspar-calcite vein occupies a breccia zone within the granite, and also contains local concentrations of pyrite, chal copyrite and pyrrhotite. "Narrow" barite veins parallel the main vein. A series of quartz veins containing disseminated to semi-massive pyrite are hosted within the granite gneiss at the Northern Creek Zone. Stripping and trenching was undertaken in 1987 and 1988 by Mr. Peter Moses. Fluorspar is reported to reach concen trations of up to 159fc of the vein. A number of barite occurrences are found within the Nipigon Bay area. The descriptions of these occur rences are derived from Tanton (1931). In the northeastern corner of Nipigon Township, (lot 9, concession 3), barite veins, between 0.3 and 0.5 m in width, trend northeasterly through Archean granite. These veins dip 800 to the northwest and can 20 be traced for 50 m. The veins consist of approximately 909fc barite, 59fc galena, 4^o sphalerite, 19fc chalcopy rite and approximately 0.5 ounces per ton silver. The following five occurrences are grouped in the Mazokama Bay region, of which the last three are within 5 km of Ozone Siding. On claim TB 6038, a calcite vein containing minor amounts of quartz, amethyst and barite cements a 10 to 13 m wide easterly-trending, shatter zone host ed within a pegmatitic granite gneiss. This zone dips steeply to the north. Calcite accounts for approxi mately 809fc of the vein material. A vein system, consisting of a network of quartz and barite veinlets, cements a 3 m wide breccia zone in trending 003 0 through arenaceous tuff, on claim TB 4588. The vein material consists predominantly of white quartz, amethyst, white calcite and rose-coloured barite. Sulphides, including galena, pyrite, chalcopy rite and sphalerite, account for up to 396 of the rock. On mining claims TB 3745/TB 4737/TB 3727, a vein system strikes 165 0 to 1770 through a pegmatiticgranite gneiss. This vein cements a 10 m wide breccia zone that dips 700 to the north. The system consists of quartz and barite veins, less than 0.3 m in width. Where the western extension of this system is exposed, barite accounts for up to 709fc of the vein material. White quartz amethyst and approximately 109fc gale na and sphalerite account for the remainder of the vein material. Minor chalcopyrite and pyrite occur dis seminated throughout the vein. A vein system, trending 087 0 and dipping 700 to 800 south, occupies a fault zone cutting pink tuff of the Sibley series at mining location TB 4533. The vein consists of approximately l m of vein material free of host-rock fragments and l m of brecciated country rock cemented with vein material. Tanton describes the vein as consisting of predominantly coarse white calcite, with lesser amounts of barite, white quartz, amethyst and purple fluorspar. Sphalerite occurs in local masses accounting for up to 39fc of the rock. Fine disseminations of galena occur throughout the calcite. A solid barite vein of up to 0.6 m is located about 3 km north of Ozone Siding. This vein forms part of a 3 m wide cemented breccia zone within granitic gneiss, striking 1000 and dipping 68 0 to the north. Quartz and sparsely disseminated pyrite occur with the barite. Hemlo Area Barite The Hemlo area barite occurrences represent the largest known barite deposits in the province, con taining over 6.5 million tonnes of barite. The Hemlo area occurrences extend from the Hem- Barite and Fluorspar in Ontario lo gold deposit, located 7 km east of the town of Hemlo, to Pic River located 22 km west of the town of Hemlo, and currently consist of six known barite deposits, most of which are located on strike with or form part of the Hemlo gold ore zone. These loca tions are shown in Map 4. The area is underlain by a highly deformed Archean metasedimentary and metavolcanic sequence as well as Archean granitic rocks. The barite occurs in massive form or as thin wispy layers interlayered with recrystallized quartz, albite, pyrite, molybdenite and carbonaceous material. The barite horizons range from l to 3 m in thickness. Accessory minerals include green mica, carbonate, and magnetite-ilmenite (Gliddon 1985). Hemlo Gold Deposit In the Hemlo gold camp, barite is found at the con tact between metasedimentary rocks and the felsic crystal tuffs, (Patterson 1984). At the Williams, Golden Giant and David Bell mines, the baritic horizon forms part of the gold ore zone. Reported ore reserves of these deposits, as of February, 1990, were 34 million tonnes, 17 million tonnes and 7.1 million tonnes respectively. Friesen et al. (1985) reported that 10 to 13*26 of the ore zone in the William mine is barite, totalling approximately 3.4 to 4.4 million tonnes. The baritic portion contains quartz and minor amounts of pyrite and molybdenite. Approximately 14*2fc of the ore zone at the Golden Giant Mine is barite and less than 59fc of the ore at the David Bell Mine is barite. A total of approximately 6.5 million tonnes of barite is estimated to be in the ore zone of the three mines. Western Occurrences: Hemlo Belt The barite occurrences form a narrow zone appar ently conformable on a regional scale with the local stratigraphy, occurring near the contact between the mafic metavolcanic rocks to the south and intermedi ate and felsic metavolcanic rocks to the north. The occurrences strike 095 0 and dips 800 to the south. The Northern Eagle Mine occurrence is located 15 km west of Hemlo, and consist of a l to 2 m thick massive barite unit striking 1100 and dipping 800 to the south. The pale grey to white barite contains thick carbonate-rich or pyrite-rich layers, which account for up to 10*fc of the rock. (Patterson, 1984). Two types of barite are found on the property: 1) massive and predominantly monomineralic, recrys tallized barite; and 2) laminated to wispy barite horizons, containing fine-grained pyrite and possibly PIC TP Cal Dynamics Energy Corporation and Kadrey Energy Corporation LECOEUR TP BOMBY TP MAP 4. Barite Deposits in the Hemlo Area. Barite and Fluorspar Resources in Ontario 21 carbonaceous material, in dark grey to black streaks. The wispy to laminated barite horizon consists of lay ers of barite, quartz-albite and pyrite-barite-carbonate in gradational contact. These layers are generally less than 2 to 3 mm thick and have undergone recrystal lization. Accessory minerals within the laminated barite horizon include green mica, calcite, magnetiteilmenite and titanite. The Padre Resources Limited property, located 17 km west of the town of Hemlo consists of a l m wide barite horizon, containing up to 709fc barite along with minor amounts of pyrite, quartz, and carbonate (Pat terson, 1984). The barite horizon strikes 1100 and dips steeply to the south. A green mica-schist, stratigraphically locat ed beneath the barite, contains minor amounts of fluorspar. Cataclastic zones within the barite horizon contain fragments of wall rock and lamprophyres. The massive barite is pale grey to white, fine grained and displays a sugary texture. The barite occurs as recrystallized, anhedral aggregates within a fine grained barite-albite-quartz matrix. Accessory minerals include pyrite, green mica, carbonate and titanite. The Rideau Resources property is located 18 km west of the town of Hemlo. A barite-bearing chert horizon, intercalated with green mica-schist, strikes 1100 across the property and dips 800 to the south. Barite occurs along with chert, albite, minor car bonaceous matter, ankerite, calcite and pyrite as microcrystalline matrix material in the recrystallized, 3.5 m wide, chert horizon. The Nexus Resources property, located 13 km west of the town of Hemlo, contains a 6 m wide, light grey baritic horizon intercalated with argillaceous metasediments (Mackie 1984). A 2.8 m wide barite-rich unit outcrops near the claim boundary between Kadrey Energy Corporation property and that of the Cal Dynamics Energy Cor poration, 22 km west of the town of Hemlo. The unit consists of light grey to white, massive barite, which grades into minor layers of pyrite-chert-carbonate. The horizon strikes 085 0 and dips 800 to the south. Three parallel barite units, up to 3 m in width, are spatially associated with the sericite-green mica schist (Patterson 1984). 22 Occurrences in Northeastern Ontario Although several minor fluorspar occurrences have been reported at various sites, the region is best known for its worked vein deposits of barite; the sole cur rent producer of barite in the province is located at Matachewan. The occurrences of barite and fluorspar are shown in Map 5. Yarrow Township Barite The only currently active barite producer in Ontario is Extender Minerals Limited in Yarrow Township. The property consists of four veins, occupying curved faults hosted within the Gowganda conglom erates and arkosic sedimentary rocks. These faults trend in an easterly direction, perpendicular to the northerly-trending Mistinikon River fault. The veins consist of approximately 609fc barite with minor con taminants of quartz, calcite and hematite. The four veins, referred to as the Southern Vein, Main Vein, Northern Vein and Creek Vein, are either vertically-ori ented or dip steeply (greater than 800 ) to the north. The veins tend to vary in width from less than l m to 10 m and often pinch out at both depth and dis tance away from the Mistinikon River fault. Although much of the Main Vein has been mined, it originally reached widths up to 10m and extended along strike for 61 m to a depth of at least 30 m. The minimum mineable width is currently l m. Ore is removed from not only the four veins on the Yarrow Township Property but also from barite veins within the local area, including the Biederman-Browning Lake vein in Cairo Township and the Tionaga (Ravena) vein in Penhorwood Township. Removal of ore from the Tracy Lake vein in North Williams Town ship is planned in 1991. Langmuir Township Barite The former Premier Langmuir Mine is located 32 km southeast of Timmins in Langmuir Township. The property contains two barite veins hosted within Kee watin mafic volcanics. The main vein averages l m in width and strikes approximately 2900 . Widths up to 2 m are recorded along the 366 m length of the vein. A second vein, located 20 m from the first, ranges in width from l to 2 m over a distance of 24 m. The vein is approximately 61 m in length. Both veins are vertically-oriented and consist of coarsely crystalline barite, calcite, minor quartz and Barite and Fluorspar in Ontario Barite and Fluorspar Resources in Ontario 23 fluorite, with traces of galena, sphalerite, chalcopyrite and native silver. Sampling by Peerless Canadian Explorations Ltd. along a 34 m length of the main vein yielded an aver age grade of 68.99fc BaSCU over a width of l m. Pyke (1970) reports that 336 tons of ore material per verti cal foot could be mined, assuming a minimum mining width of 1.6 m over a length of 183 m at a grade of 559fc BaSO4. An estimate of 250 tons per vertical foot could be mined from the second vein, at a minimum mining width of 1.6 m over a distance of 137 m for ore grading 559fc barite. Penhorwood Township Barite The Tionaga deposit in Penhorwood Township is 4.8 km west of Tionaga Station on the C.P.R. Line north of Capreol. It is also known as the Ravena deposit. The property is underlain by pink Algoman granite, which has intruded mafic volcanics and sed imentary rocks including iron formation. The main barite vein occurs in a northeasterlytrending vertical fracture, parallel to a weakly developed joint system within the granite. The vein reaches widths of up to 5 m, but averages 2 m over a distance of 30 m. The vein extends over a distance of approximately 150 m, although the central portion pinches out on surface. A second vein located 12m west of the main vein averages 0.6 to 1.3 m in width. According to Guillet (1963), the vein consists almost entirely of barite. The barite is massive, white and generally fine-grained. Coarsely crystalline barite occurs scattered throughout the finer-grained matrix. Contaminants such as calcite and purple fluorspar tend to be restricted to a 15 cm zone adjacent to the wallrock. Spence (1922) reports that ten channel samples, taken across the main vein, average 959fc BaSCM. The second vein contains 989e BaSO-t. A 472 kg bulk sam ple analyzed by the St. Joseph Lead Company yielded 96.1496 BaSO4 and t.89% SiO2 . zone reaching a maximum width of 0.75m. "Small amounts" of galena, sphalerite and chalcopyrite give the barite a pinkish colour (Spence 1922). A sample, representative of the entire vein width, yielded 74.859fc CaCOa. Another sample, representing 2.5 m across the vein, assayed 90.509c BaSO4 (Burrows 1918). Lawson Township Barite A vertically-oriented lens of barite strikes 75 0 through the Proterozoic Nipissing diabase, 1.7 km southeast of Longpoint Lake in Lawson Township. The lens is 18 m in length and 2.5 m in width. Vein material has been removed along its entire length to a depth of 2.5 m. The vein strike parallels one of the two joint directions in the diabase. Spence (1922) claims that the vein is practically free of sulphides and fluorite. The vein consists of both fine and coarsely crystalline barite. Spence reports a grab sample assaying 98.039c BaSO4, G.70% SrSCu, and 1.209c CaCOs. North Williams Township Barite The Tracy Lake barite property contains two barite veins trending northeasterly through arkose of the Lorrain Formation. A trenching programme under taken in 1977 by Extender Minerals Limited determined that the "A" vein had a strike length of 228 m while the "B" vein had a strike length of 457 m; portions of the vein with a width greater than l m were 137 m and 70 m in length respectively (Ministry of Northern Development and Mines Assessment Files). Some portions of the veins are up to 2.4 m in width. Drilling undertaken in 1977 by Extender Min erals indicated that the "A" vein dipped 82 0 south. Assays of 13 samples of vein material between the year 1975 and 1977 indicated that the content ranged between 95 and 999c barite, with one sample assaying 68*?fc barite and another sample assaying 899b barite (Ministry of Northern Development and Mines Assess ment Files). Cairo Township Barite The Biederman deposit in Cairo Township is on the west shore of Browning Lake, approximately 8 km northeast of the town of Matachewan. The property is underlain by a hornblende syenite (Spence 1922). The vertically-oriented, northwesterly-trending barite vein reaches a maximum width of 5 m. The vein can be traced for a distance of approximately 30 m. Purple fluorspar occurs along the walls of the vein. The main contaminant is quartz, which occurs as an acces sory mineral throughout the vein and as a quartz-rich 24 Barite and Fluorspar in Ontario Occurrences in Southeastern Ontario The most numerous fluorspar occurrences in the province are found in the southeastern region, partic ularly within Madoc, Huntingdon, Cardiff, Monmouth and Ross townships. Many of the barite vein deposits are located in Frontenac, Hastings and Lanark counties. Barite also occurs in association with some of the Madoc-Moira Lake fluorspar veins. Much of the barite in the region, how ever, occurs in relatively thin veins in comparison to those of the Thunder Bay and Matachewan areas of Northern Ontario and is not considered in detail in this section. Map 6 shows the location of fluorspar and barite occurrences in southeastern Ontario. Guillet (1963, 1964) provides a detailed description of individual occurrences. Madoc-Moira Lake Area Mining was conducted in the area from 1905 to 1961 and, while no production has occurred since 1961, research into locating additional deposits has continued sporadically up to the present day. The most productive fluorspar veins within the province are located in the Madoc-Moira River area. They occur as fracture-fillings along two northwesterly-trending fis sure fault systems covering a distance of approximately 154 km and spanning a width of approximately 5 km. The veins occur sporadically along both fault systems (Wilson 1929) as well as along joints and fissures within the country rock, which have undergone little movement (Williams and Thompson 1986). Although most of the fluorspar occurrences are located within the Palaeozoic limestone, the largest occurrences and most productive mines were located within the Precambri an marble and granite. The vein deposits of the Madoc-Moira Lake area, and related geochemical/geological data, are shown in Map 7. A survey to assess the fluorite potential of the Madoc and Cardiff Township areas was carried out between 1941 and 1951 by the Geological Survey of Canada. This survey involved making evaluations of the grades of ore remaining at a number of the pastproducing mines in the Madoc area. Programs undertaken during this survey involved bulk sampling, diamond drilling and beneficiation testing. The results of the drilling program on the Keene, Perry, Coe, Rogers, Bailey, Johnston, Mcllroy and Kilpatrick prop erties are summarized in Guillet (1964). The best Barite and Fluorspar Resources in Ontario intersection was on the Keene property and comprised 2.96 m grading between 55 and 609fc CaFi over a true width of 3.18 m. The thickest vein widths on the Per ry property are located near shafts number 2 and 3, and only minor veinlets were observed in the core drilled on the Coe property. On the Kilpatrick property, vein material obtained in the core graded on average between 50 and 859fc CaFi. Vein widths are estimated to reach their greatest true widths at 1.89 m, but much of the core was lost when drilling through the vein. A fluorspar vein can be traced over a distance of 335 m on the Johnston property. The vein pinches and swells with maximum true width reaching 2.26 m with a grade of 45 ^c CaF2. Only a minor amount of fluorspar was observed in the drilling of the Mcllroy property. Vein material could be traced for 348 m across the Rogers property. The vein pinches and swells with a maximum true width reaching 1.24 m, grading 60*36 CaFz. Again, lost core was common, making true vein widths difficult to determine. On the Bailey property, the vein averages 7.07 m in width over a distance of 70 m; the materi al from the Wallbridge, Howard, Coe, Keene, Bailey and Johnston properties indicate that the ore can be up graded to a product containing between 71 and 939fc CaF2 through simply jigging, tabling and calcine processing. A number of regional normal faults in the area strike parallel to the major rift zones of the region. Surface traces of these faults tend to be distinctly curved, espe cially at junctions with other faults (Thompson and Williams 1987). The fluorspar deposits of the Madoc area occur either as connected lenses, disconnected en echelon lenses or isolated lenses within faults or fractures in Palaeozoic or underlying Precambrian rocks. The largest ore bodies occur where the rock has failed along a single fracture (Guillet 1964). Wilson (1929) recognized the presence of two fault systems: one striking 115 0 and representing a predominantly hori zontal fault motion and one striking 135 0 representing a vertical to sub-vertical fault motion. Because most of the veins with the second orientation were geo graphically removed from those belonging to the Moira Fault system, Wilson referred to this group as the LeeMiller Group, which nearly all lie in concession l, Madoc Township. Guillet (1964) proposed that the lenticular cavities occupied by the fluorspar-bearing veins were caused by the horizontal displacement of the walls on an undulating fault surface. Recent mapping and geophysical work (Thompson 1989; Thompson and Williams 1987, 1988, 1989; Williams and Thompson 1986), confirms the existence 25 26 Barite and Fluorspar in Ontario D 0 5 0 O g o i o o •o D ^ c w O CL 0 IX O. Barite and Fluorspar Resources in Ontario 27 of the two distinct fracture systems. They concluded that displacement along fluorspar-bearing fractures was not generally significant. They propose that the fluorspar-bearing veins occupy fractures adjacent to faults and that the largest deposits have been located close to fault junctions. Their work has led to a revi sion of the classification of the Palaeozoic rocks in the area and to the identification of a major volcanics at the O'Kara Mill site. A number of the fractures trend ing 1350 in the vicinity of the Moira fault system were also recognized. It is uncertain whether the two fracture patterns were produced during one deformation event or two separate events; whether the emplacement of vein material took place during one or two episodes and whether one fracture system is filled with vein mate rial of a higher grade over the other. The three largest producing mines Rogers, Bailey, and Noyes fall along both fracture systems, with the Noyes Mine being located at the junction of both systems. Detailed geological and geochemical surveys were recently undertaken in three sub-areas within the immediate Moira Lake area (Dickson and Trinder 1989). The surveys confirmed the distribution of rock types previously determined by Hewitt (1968), Lalonde (1974) and Thompson (1986). The results of the geo chemical surveys identified several coincident fluorine-barium-zinc target anomalies. Trenching of some of these targets failed to reveal any fluorsparbarite vein material on surface. The vein material consists of fluorspar, calcite, barite and minor amounts of celestite, quartz, marca site, pyrite, sphalerite and other sulphides (Guillet 1964); it tends to occur as either alternating bands or as irregular network partitions between vein cavities (Wilson 1929). Although the vein minerals tend to occur intermingled or interlayered in various propor tions with no apparent order of precipitation, they often occur as two parallel mineral zones separated by a zone of fractured country rock. The zor, j -.re usually of uneven width, the separating zone of coun try rock ranging from a few centimetres to several metres in width (Wilson 1929). Lenses within the vein system range from less than l to 60 m in length and from under l to 5 m in width. Lenses of vein materi al tend to extend diagonally along the vein strike. According to Guillet (1964), there appears to be no consistent order of crystallization; however, quartz, sulphide minerals, and celestite tend to occur near to the wall of the veins. The banded distribution of fluorspar, calcite and barite indicates a rhythmic mode of deposition (Guillet 1964). Although the composition of the vein material is 28 extremely variable, Guillet (1964) reports that the Madoc ore averages between 50 and 7596 fluorspar. Calcite constitutes 25 to 5096 of the veins and barite ranges between 5 and 4096, but averages 1596. Celestite, quartz and sulphide usually account for less than 596 of the vein material. According to Guillet (1964), the calcite content of the vein increases with both depth and narrowing of the veins, at the Howard, Keene and Bailey Mines. Many of the "granitic" plutons within the MadocMoira Lake area are enriched in fluorine (Wu 1984). Phases of the Deloro pluton have fluorine contents that range from 1000 to 3660 ppm. The Barber Lake granite, located 20 km northeast of Sharlot Lake, and the Cheddar granite, located southeast of Bancroft, are both enriched in fluorine (Wu 1984). Lalonde (1974) has documented enriched fluorine contents in the marbles and siliceous rocks adjacent to the Deloro pluton. Easton (1989) proposes that the Moira Lake gran ite is connected to the Deloro pluton at depth, and that it may be the source of some or all of the fluorine found within the fluorspar-calcite-barite veins in the Moira Lake area. Cardiff, Monmouth, and Ross Townships Fluorspar veins are hosted within the northeaster ly-trending metamorphosed alkalic suite of intrusive rocks that extends over 100 km in length from Ross Township in the north to Glamorgan Township in the south. This suite consists of alkalic granite, alkalic syenite, nepheline syenite and mafic alkalic rocks (Lumbers 1982). Cardiff Township Fluorspar There are ten main fluorspar occurrences in Cardiff Township. Fluorspar occurs as a major constituent of narrow, lensoidal veins, hosted within the syenitic pegmatite and gneiss (Guillet 1964). Recent mapping by Bright (1983) has indicated that many of the fluorspar veins have a spatial association with car bonate dikes or lenses (possibly carbonatites). The fluorspar in both Cardiff and Monmouth Town ships occurs in fluorspar-calcite-apatite veins. These veins are described by Guillet (1964) as being irreg ular, discontinuous bodies, ranging in width from a few centimetres to 0.3 m and up to 100 m in length. The veins are highly variable in both composition and size along strike and down-dip. The dark purple fluorspar generally accounts for 20 to 3096 of the vein material (Guillet 1964). Along with the major miner als of fluorite, calcite, and apatite, local concentrations Barite and Fluorspar in Ontario of hornblende, biotite, pyroxene, scapolite and mag netite can occur. The major minerals often occur as well-banded purple fluorspar, grey to cream-coloured calcite, and pale pink calcite (Satterly 1956). Postdepositional motion along the faults hosting the veins result in the development of a finely-banded, mylonitized calcite-fluorspar material. Uranium-bearing minerals are present in the fluorspar veins at the Cardiff-Fluorite, Richardson, Tripp, Clark and Montgomery properties. Radioactive minerals have not been recorded at the Dwyer, Schickler and the Number 3 Zone of the Richardson properties (Guillet 1964). Monmouth Township Fluorspar A number of fluorspar occurrences are located in the east and southeastern portion of Monmouth Township. Most of these occurrences are small; however, dia mond drilling carried out between 1971 and 1975 by Landair Exploration Limited outlined approximately 2 million tons of low-grade fluorspar ore in calciteapatite-fluorspar veins, containing uraninite, uranophane and titanite, on a property extending between Concessions X to XII and Lots 33 to 35 (Mar tin 1983; Bright 1987). This occurrence consists of two fluorspar horizons covering a length of 617 m and a width of 4 m. An upper horizon consists of calcite and fluorspar veins hosted within a granite pegmatite. The main vein of this horizon averages 2 m in width and contains between 20 to 249fc CaFi (McConnel, 1977). A lower horizon consists of several narrow calcite-fluorspar veins occurring across a stratigraphic width of 5 to 9 m (Martin 1983). Ross Township Fluorspar Six fluorspar occurrences are hosted within the alkalic complex that underlies much of the western portion of Ross Township. All occurrences consist of fluorspar-calcite-apatite veins hosted within the syenitic gneiss (Satterly 1945). Commentary Although most of the showings and shallow work ings of fluorspar and barite in the province have been well documented in the past, notably in the reviews by Guillet in the sixties, it is also true that such occur rences have rarely been further explored to investigate the possibilities of economic reserves. Metals exploration programs in recent years have led to the incidental discovery of significant deposits in terms of volume, for example, Hemlo Belt barite and Springpole Lake fluorspar. Such discoveries encour age the view that concentrations at depth of potential economic interest for either of these two minerals remain to be identified in Ontario. Moreover, the pre sent-day viability of working small deposits for specialty markets has been successfully demonstrated by the extraction of vein barite since 1967 by Exten der Minerals of Canada Ltd. in the Matachewan area near Timmins. This review has drawn attention to the more promi nent showings, both individual deposits and clustered occurrences, which may merit further investigation. It has also noted the spatial association of several occurrences with alkalic igneous rocks and associat ed carbonatite intrusions that merits the attention of explorationists. On the basis of the geological infor mation reviewed to date, the following areas are highlighted for their actual or potential resources: Barite Thunder Bay area, N.W. Ontario Vein-type occurrences have been worked commer cially during the last century for their barite content or for attendant silver values. The southern vein sys tem, along a line of islands including Jarvis, Thompson, Spar and McKellar Islands, has recorded vein widths of up to 21 m. The grade of barite with in the veins is high, between 84 and 909fc BaSO4 where documented. The only stated estimate of barite reserves is for McKellar Island at 50,000 short tons. The north ern vein system is less well documented, but veins up to 6 m wide are noted, with probable grades of above 80*?fc BaSO4 for the barite in O'Connor Township. A combination of three or more deposits in these vein systems could provide an overall resource esti mate of better than 200,000 tonnes of barite. Matachewan area, N.E. Ontario Several known vein-type barite deposits, generally narrow, have been worked in an area centred on Mat achewan to the south of Timmins. These deposits, and that of Tionaga to the west, were originally worked Barite and Fluorspar Resources in Ontario 29 from surface and are now mined by underground meth ods to produce up to 25,000 short tons per year with an estimated average grade of 50 to 609fc BaSCU; the grade of the barite contained in these veins, however, is often above 909fc BaSO4 on the basis of specific samples. Hemlo area, N.W. Ontario A substantial barite resource occurs in stratiform deposits which host economic values of gold. Three operating mines currently extract approximately 10,000 tonnes of gold ore per day (Table 9) from the under ground workings. In original ore samples, a barite content of up to 1496 BaSO4 was noted, but current mined ore grades appear to be below 109fc BaSO4. The ore also contains molybdenite, pyrite and stib nite. At present, only gold is recovered in the three operations. The processing plant residues, which are finely ground, are deposited together with water in adjacent tailings ponds. The gold ore reserves are large and are expected to sustain production at these oper ations for many years at current production rates. Fluorspar Madoc-Moira Lake area, S.E. Ontario Numerous fluorspar veins, principally located with in two vein-fault systems, have been worked from early in this century up to 1961. Total reported pro duction from 1905 to 1961 of metallurgical grade fluorspar was around 110,000 tonnes. The veins, which include varying amounts of calcite, quartz and barite, have yielded samples of over 709fc CaFz, but an aver age grade of 409fc to 6096 CaFz is more probable. The literature does not provide any formal estimates of reserves for the individual deposits. An undetermined amount of ore is known to be present below mined depths and along vein extensions. alkaline rock assemblages that is found across the province and encourages the targetting of this miner al in future exploration programs within these rock suites. In summary, the great majority of individual occur rences of barite and fluorspar in the province are small vein deposits. In such cases, as demonstrated by the current operations of Ontario's barite producer, several of these deposits would be needed to provide adequate tonnage to a central milling operation to offer eco nomic potential. Exploration in the short term should begin with the known vein systems in suitable prox imity of prospects. Examples are the Thunder Bay vein-fault systems for barite and the Madoc-Moira Lake vein systems, as well as the occurrences in Cardiff and Monmouth townships for fluorspar in east ern Ontario. The available evidence for reserves in these vein deposits is scant; nevertheless, exploration targets of over 200,000 tonnes of barite in the Thun der Bay area and of over 500,000 tonnes of run-of-mine fluorspar ore from a variety of eastern Ontario deposits should be considered as objectives for speciality markets. The two major known deposits in Ontario at the present time, in terms of indicated or proven volumes, are both gold properties in northwestern Ontario. The Springpole Lake gold prospect is still in the explo ration stage, but significant fluorspar values will contribute to the economic evaluation of the property. The gold ore zone mined at Hemlo includes substan tial quantities of barite. In light of strong regional market demand for each of the industrial mineral com modities for high-value chemicals production, it would be opportune for mining companies to review the pre sent economics of by-product recovery potential for such minerals. Red Lake area, N.W. Ontario The Springpole Lake carbonatite body to the north east of Red Lake includes significant fluorspar mineralization in terms of volume and grade, accord ing to recently reported drilling results. This is a prominent example of fluorspar in association with Table 9 Hemlo Area Daily Gold Ore Production Golden Giant Mine Hemlo Gold Inc. David Bell Mine Teck-Corona Corp. Williams Division Corona Corp. 30 3000 t/d 1100 t/d 6000 t/d Barite and Fluorspar in Ontario 3. Options for Barite Mineral Production Existing Production Production of barite is currently limited to one com pany in the province. The company, Extender Minerals of Canada Ltd., produces barite ore from two mines in North-Eastern Ontario in the townships of Penhor wood and Yarrow from underground vein deposits (Andrews and Ceilings 1990; Collings and Andrews 1988a; Guillet and Kriens 1984). Mining methods are simple and low-key with a minimum of personnel. Approximately 25,000 (short) tons per annum of barite ore is partially upgraded at the mine sites, then trucked to a finishing plant in Matachewan. In this plant, the ore is dried and finely ground prior to bagging for sale in the mineral filler industry. The finished grade of barite is approximately 969fc BaSO4. Ore produced from the two mines is between 50 and 609fc BaSCU before treatment. This operation has been continuous for a number of years and seems to fit a market niche, probably with long term contracts. It is probable that the deposits being worked could sustain a higher level of produc tion if demand were proven and following some extra development of the underground workings or adjacent veins not presently being worked. The grade of mate rial being sold is suitable as feedstock for a barite chemicals plant. It is not known what level of recov ery is maintained in the upgrading process. Production Options A major use of barite is for drilling mud and this demand is met by a number of large volume, low-cost producers. Although the specifications for drilling mud barite are a little less rigid than for chemical grade barite, production of drilling mud grade mate rial from Ontario sources is not considered to be practical due to the type of mineral resources and the implied control of the market by the existing producers. A possible market is considered for up to 30,000 tonnes per year of chemical grade (92 to 969fc BaSO-O barite, as feedstock for a chemicals plant producing a range of barium compounds. This demand could be satisfied by: * A single mill producing 30,000 tonnes per year of finished barite * Two or more mills sized for smaller production from different areas in the province * A single mill producing 30,000 tonnes per year of barite as a by product of the Hemlo gold mines. The accepted specifications (Griffiths 1988) for chemical grade barite are given in Table 10. Options for Barite Mineral Production 31 An average of 949fc BaSCU is considered in the fol lowing production discussions. These options are examined as follows: 30,000 tonnes per year Barite Mill The Thunder Bay area appears to have the required in-situ ore grades and volume of deposits necessary to support a processing plant producing 30,000 tonnes per year of finished (average 9496 BaSCU) barite. An area reserve of at least 150,000 tonnes (of equivalent contained barite) would be required to initiate devel opment of a project. From the data presented in available reports, it seems unlikely that a single vein deposit could sustain this level of production. After allowing for average mined ore grade and mill recovery, a mill feed rate of 47,000 tonnes per year would be required. The deposit on McKellar Island has a stated reserve of 50,000 (short) tons (Ceilings and Andrew 1988a), but extraction rates would be limited by access to the site and the few possible working places on the surface of the small island. Possibly an underground operation would allow a higher production rate but development would be costly. An individual production rate of 10,000 to 15,000 tonnes per year of ore may be attained with surface workings. The neighbouring islands (Spar, Jarvis, Thompson) have similar deposits but these are not as well defined and if anything have narrower veins thus limiting production rates. It is possible that silver might occur in the barite vein structure and could be recovered during processing by gravity sep aration methods. The vein deposits of O'connor Township and the surrounding area offer easier access pending rights of way and ownership obligations. The veins here are narrower than on the islands but apparently contain high grade barite. Due to the fairly short distance between the island and O'connor Township deposits, a proposed mill for 30,000 tonnes per year production could be located centrally to treat ore trucked from two or more min- Table 10 Specifications for chemical grade barite BaSCu BaSCu CaF2(max) SrSCMmax) 92-96 (lump) 96-98 (flotation cone.) 0.5 1.0 1.0 32 ing locations. Ore from the islands would have to be transported across water by barge or possibly trucked over ice bridges during a brief period in mid-winter. The location of the mill would be selected to take advantages of existing highways, services and suit able land for the plant site and tailings disposal. Based on information concerning the deposits and preliminary test programs at CANMET (Andrews and Collings 1990), the processing of the ore from these deposits would be simple and low cost. Previous pro duction of barite depended on careful extraction from veins combined with hand sorting. CANMET studies of numerous samples showed that gravity separation alone was not always sufficient to obtain a satisfactory concentrate grade. In order to allow treatment of var ious deposits and to minimize manual upgrading, a combination of gravity concentration and flotation appears to be required. Grinding of gravity rejects pri or to flotation will allow a maximum recovery of the barite from the ore. In the proposed plant, initial size reduction of mined ore is followed by recovery using jigs and tables, fol lowed by grinding and flotation of the gravity circuit tailings. Iron containing minerals will be removed from the combined gravity and flotation product by high intensity magnetic separation and the final prod uct will be dried sufficiently to allow transport by truck to the proposed chemicals plant. Any excess production is exported. This flowsheet is illustrated in Figure 1. The two other areas of potential barite production are not considered to be as attractive for the siting of a 30,000 tonnes per year production mill. The Mat achewan area mines probably have sufficient reserves but at the lower mined grade of ore, a mill feed rate of 80,000 tonnes per year would be required. A typi cal flowsheet for this type of ore is shown in Figure 2. It is doubtful if this level of production could be eas ily obtained in addition to current activities. A substantial development program would be required ahead of the production period. The deposits in the South-Eastern part of the province are small, of vary ing grade and a substantial program of exploration would be required to determine if available reserves could sustain the desired production rate. Two or More Mills The siting of at least two mills to produce an aggre gate of 30,000 tonnes per year of finished barite appears feasible. The mills would be situated close to the mineral deposits and would suit the obtainable mining production rates. A disadvantage is the high er unit processing cost per tonne of product. For this Barite and Fluorspar in Ontario OPEN PIT MINE WASTE ROCK 80* BoS04 JAW CRUSHER TO Z' CLAY. SLIMES SIZE REDUCTION (HAUMERMIU.) l PRODUCT -1/2" SHAKING TABLES CONCENTRATE ROD MILL TO -300 urn 2 BARITE ROUGHER FLOTN. BARITE FLOTATION CONCENTRATE BARITE CLEANERS HIGH INTENSITY BARITE CONC +94X BoSO FILTRATION AND DRYING aOTATION TAILINGS CHEMICAL PLANT Figure 1. Barite Recovery from Vein Mine - Open Pit. reason the study considers two mills only, each rated at 15,000 tonnes per year of barite concentrate. A probable location for the two mills is one in the Thun der Bay area and one in the Matachewan area. This is premised on the possibility of expanded mining capac ity from the current operations near Matachewan or development of other deposits in that area. The overall production cost of barite will be high er than in the first option due to the implied additional transportation cost of barite to the chemicals plant, which would be situated either centrally or close to one of the producing areas. By-Product Mill The production of 30,000 tonnes per year of barite as a by-product from the existing gold mines in the Hemlo areas is considered. One of the mines (Golden Giant Mine of Hemlo Gold Inc.) produces a sufficient quantity of ore to sustain this proposed production. Barite would be recovered by processing a portion of Options for Barite Mineral Production the present gold mine reject (tailings) stream which is being discharged to a tailings disposal area. The grade of barite in the existing tailings stream is low and assumed for this study to average 8*?fc BaSO4- The tailings solids also contain minor quanti ties of pyrite, molybdenum sulphide and smaller amounts of other metal sulphides plus mica. Process ing methods must remove these deleterious minerals in order to produce the required high grade barite con centrate. Hemlo Gold has installed and operated briefly a molybdenum recovery circuit within the existing mill but operation was curtailed due to unfavourable economics. The obvious advantage for the proposed barite recovery plant is that all ore mining and size reduction is conducted as part of the gold recovery operation. The mill cost of barite production would still be high since approximately 705,000 tonnes per year of gold mill tailings need to be processed to yield the required 30,000 tonnes per year of barite. This is a 33 UNDERGROUND MINE WASTE ROCK 55J6 BaSO, JAW CRUSHER TO 2" l CLAY, SUMES LOG WASHER SURGE BIN SIZE REDUCTION (HAMMERMILL) w PRODUCT -1/2" BARITE JIGS CONC. BARITE GRAVITY CONCENTRATE SHAKING TABLES TAILINGS ROD MILL TO -300 urn SCREEN -300 um SUMES REJECT CYCLONE CONDITIONER BARITE FLOTATION CONCENTRATE l BARITE ROUGHER FLOTN. CONC. BARITE CLEANERS 6 STAGES HIGH INTENSITY MAG. SEPARATION BARITE CONC. +94X BoS0 4 FILTRATION AND DRYING FLOTATION TAILINGS V REJECTS V BARITE TO CHEMICAL PLANT Figure 2. Barite Recovery from Vein Mine - Underground. 34 Barite and Fluorspar in Ontario substantial quantity, equivalent to a mill capacity of about 2,000 tonnes per day. In order to produce a clean, high grade barite con centrate, the flotation process would be employed. Recovery by flotation of pyrite, molybdenum and oth er metal sulphides will be necessary prior to the barite flotation stage. Final cleaning by acid leaching will probably be required to eliminate iron contamination. The selected process is shown in Figure 3. Although not specifically included in this study, costs associat ed with possible royalties and changes to existing disposal systems may be incurred. The recovery of barite will also remove from the gold mill tailings a major source of material available for backfilling underground workings. While Hemlo Gold does not presently recover material for backfilling it is possi ble that this may be a future consideration. Production Costs The costs of barite production have been estimated on the basis of the three main production options pre viously described. The costs comprise two main categories: - Pre-production capital costs for mine develop ment, mill construction and services, * Operating cost during the production phase including transportation of ore and concentrate. Mining costs are developed on the basis of a con tracted mining operation using typical rates for small open pit or underground mines, thus reducing capital requirements. The major capital expenditure in each case is for construction of a milling facility which includes services. Mill sizes equivalent to annual pro duction levels of 15,000 and 30,000 tonnes per year are examined for each probable producing area. Direct operating costs include mining, ore trans portation and milling. Milling costs are derived from estimated labour costs plus processing costs (power and raw materials), the latter based on flowsheets and chemical consumption rates proposed in the CANMET testwork (Ceilings and Andrews 1988a). Added to the direct operating cost of barite pro duction is the cost of capital expenditure recovery and an allowance for product shipping. It is assumed for comparison that capital expenditures will be recov ered during the first five years of production. Product shipping to a chemicals plant is assumed to be by nor mal highway type truck but depends primarily on site and market locations. Open Pit Vein Production A preliminary design for the processing plant and the preliminary estimate of operating cost is premised on the assumed criteria listed in Table 11. This is typical of a Thunder Bay area plant described previously. The small proportion of operating time is Table 11 Preliminary Operating Costs for an Open Pit Barite Operation Mined ore grade Barite recovery Product grade Annual production Seasonal operation Days per week Hours per day Options for Barite Mineral Production ( 0Xo BaSO4) W ( 0Xo BaSO4) (tonnes) (months) 80 75 94 30,000 8 5 16 35 MAIN FLOW TO MILL TAILINGS POND GOLD MILL TAILING STREAM 8X Base* MOLY FLOTATION CONDITIONING MOLY ROUGHER FLOTN. CONC. MOLY CLEANERS 6-9 STAGES MOLY FLOTATION CONCENTRATE TO SALE FILTER, DRYER, DRUMMING TAILING i*——~—— CLEANER TAILINGS TO JOIN GOLD MILL TAILINGS f\ PYRITE FLOTATION \J CONDITIONING l PYRITE ROUGHER FLOTN. CONC. PYRITE FLOTATION CONCENTRATE TAILING BARITE FLOTATION CONDITIONING BARITE ROUGHER FLOTN. CONC. BARITE CLEANERS 6 STAGES BARITE FLOTATION CONCENTRATE SHAKING TABLES ACID LEACH WATER RINSE TAILINGS TO JOIN GOLD MILL TAILINGS CONCENTRATE FILTRATION AND DRYING, STORAGE V PRODUCT TO CHEMICAL PLANT Figure 3. Barite Recovery from Mill Tailings. 36 Barite and Fluorspar in Ontario Table 12 Mine and mill production cost summary Barite mill, open pit vein mine ANNUAL COST, S Payroll Reagents and Supplies Maintenance Supplies Power and Fuel Contract Mining Ore Haulage to Mill (40 km) Insurance, taxes, etc. General Contingency Direct Operating Cost Capital Repayment (5 years) Product Shipping (40 km) Total Production Cost 582,000 243,000 75,000 160,000 644,000 460,000 50,000 115,000 232,900 2,561,900 600,000 78,000 3,239,900 UNIT COST, S/t ore 12.65 5.28 1.63 3.48 14.00 10.00 1.09 2.50 5.06 55.69 13.04 1.70 70.43 UNIT COST, S/t Product 19.40 8.10 2.50 5.33 21.47 15.33 1.67 3.83 7.76 85.40 20.00 2.60 108.00 NOTE: Milling Rate = 46,000 tonnes per year Product Rate - 30,000 tonnes per year selected to suit seasonal production and handling of the open pit ore and to optimize the fixed labour costs. The estimated capital cost for this facility is approx imately S3 million. Mining equipment is not included as costs are based on a contracted mining and ore haulage operation. Preliminary information on the sizes of major items of equipment and typical pur chase costs are provided in Appendix A. The estimated production cost is developed in Table 12, resulting in a direct operating cost of 385 per tonne of barite product. Indirect costs for capital recovery and product shipping are estimated to bring the over all production cost to approximately S108 per tonne of barite. Silver may also be recovered when working favourable vein deposits and sold as a by-product, thereby reducing net operating costs. A total of 14 personnel are required for operation Table 13 Estimated costs for a 15,000 tons per year open pit operation Capital cost Direct operating cost Overall production cost S3 million S108 per tonne barite S151 per tonne barite Options for Barite Mineral Production of the plant, plus contractors engaged in mining and trucking. The capital cost of a facility to produce 15,000 tonnes per year of barite is estimated to be similar, based on the use of an identical plant but at reduced operating time. The operating cost will be slightly higher due to the effect of the lower production rate on fixed costs. At 15,000 tonnes per year capacity, the total esti mated costs are shown in Table 13. Underground Vein Production A similar processing plant is proposed for upgrad ing underground ore from a typical North-Eastern Ontario producer. Table 14 illustrates the criteria employed. Operation during a 12 month per year period is pro posed due to the higher ore treatment rate and to avoid stockpiling ore during winter periods. The estimated capital cost for the facility is again approximately S3 million. This plant can be identical to the plant employed to treat the open pit vein deposits. A preliminary estimate of direct operating cost is S159 per tonne of barite, with an overall pro duction cost (including capital recovery) of S242 per tonne barite produced. This is shown in the Table 15. It has been assumed also that the product will be 37 Table 14 Table 16 Preliminary operating costs for an underground barite operation Average Operating Cost for Two Mills Mined ore grade ( 0Xo BaSO4) Barite recovery ( 0Xo) Product grade 0Xo BaSO4) Annual production Seasonal operation months Days per week Hours per day 55 70 94 30,000 12 5 16 shipped to a chemicals plant located either in NorthEastern Ontario or in Southern Ontario. A total of 15 personnel are required, plus contractors engaged in mining and trucking. At the lower production rate of 15,000 tonnes per year, which may be more applicable in this case, the capital cost remains as S3 million and the overall pro duction cost increases to S274 per tonne barite. Two or More Mills The concept of two or more mills producing an aggregate of 30,000 tonnes per year of barite may suit the proposed production rate from the presently known deposits. On the assumption that a mining/milling Capital cost (2 mills) Operating cost (direct) Operating cost (overall) SG million S146 per tonne barite S212 per tonne barite operation of the two types considered above may be combined, an average cost is shown in Table 16. This overall cost implies the shipment of half of the production over a considerable distance to a chem icals plant located near one of the producers. Total employment related to the two plants is estimated to be 23, plus personnel engaged in contract mining and trucking activities. By-product Recovery A processing operation designed to recover 30,000 tonnes per year of barite from gold mill tailings in the Hemlo area needs to process approximately 705,000 tonnes per year of the tailings. The proposed plant will treat a portion of the current tailings stream, with design criteria shown in Table 17. Continuous operation throughout the year is designed to match the gold mill operation. The option of recovering already deposited tailings is not con- Table 15 Mine and Mine Production Cost Summary Barite Mill, Underground Mine ANNUAL COST, S Payroll Reagents and Supplies Maintenance Supplies Power and Fuel Contract Mining Ore Haulage to Mill (40 km) Insurance, taxes, etc. General Contingency Direct Operating Cost Capital Repayment (5 years) Product Shipping Total Production Cost 734,000 328,000 50,000 184,000 2,080,000 800,000 50,000 115,000 434,100 4,775,100 1,000,000 1,485,000 7,260,100 UNIT COST, S/t ore 9.18 4.10 0.63 2.30 26.00 10.00 0.63 1.44 5.43 59.69 12.50 18.56 90.75 UNIT COST, S/t Product 24.47 10.93 1.67 6.13 69.33 26.67 1.67 3.83 14.47 159.17 33.33 49.50 242.00 NOTE: Milling Rate = 80,000 tonnes per year Product Rate = 30,000 tonnes per year 38 Barite and Fluorspar in Ontario Table 17 Design Criteria for By-product Recovery Capital cost S3 million Ore grade-gold mill tailings ( 0Xo BaSO4) 8 Barite recovery (0Xo) 50 Product grade ( 0Xo BaSCU) 94 Annual production 30,000 Seasonal operation months 12 Days per week 7 Hours per day 24 18, giving a direct cost of approximately S100 per tonne of barite product. The addition of indirect costs for capital repayment and product shipping brings the total production cost to approximately S180 per tonne. Molybdenum sulphide may be recoverable for sale as a by-product, thereby reducing net operating cost. A total of 17 personnel are required for plant oper ation and administration. sidered due to the difficulty and cost of working with in the tailings pond areas. It must be noted that, while the area is developed by the existing mining operations, a new independent facility would still require development of the site and installation of services. The exception would be if one of the existing gold producers installed a barite recovery plant as an adjunct to the present milling operation. This has not been considered for this study. The capital cost of the facility is estimated to be approximately S8.4 million. Preliminary information on the sizes of major items of equipment and typical purchase costs are provided in Appendix A. The estimated production cost is developed in Table Table 18 Mine and Mill Production Cost Summary Barite Mill, Gold Mill Tailings ANNUAL COST, S Payroll Reagents and Supplies Maintenance Supplies Power and Fuel Contract Mining Ore Haulage to Mill Insurance, taxes, etc. General Contingency Direct Operating Cost Capital Repayment Product Shipping Total Production Cost 835,000 955,000 300,000 393,000 0 0 100,000 105,000 268,800 2,956,800 1,686,000 757,200 5,400,000 UNIT COST, S/t ore 1.18 1.35 0.43 0.56 0.00 0.00 0.14 0.15 0.38 4.19 2.39 1.07 7.66 UNIT COST, S/t Product 27.83 31.83 10.00 13.10 0.00 0.00 3.33 3.50 8.96 98.56 56.20 25.24 180.00 NOTE: Milling Rate a 705,000 tonnes per year Product Rate = 30,000 tonnes per year Options for Barite Mineral Production 39 40 Barite and Fluorspar in Ontario 4, Options for Barium Chemicals Production Options for Barium Chemicals Production Production Options The majority of barium chemicals are derived from high quality barite ore, containing a minimum of 949fc barium sulphate (BaSO4), which is reacted with a car bon source (usually coal) at high temperature to produce barium sulphide, the precursor of a wide range of barium chemicals. Primary and secondary deriva tives of the BaS that were identified as representing a potential commercial opportunity for Ontario's indus trial minerals industry include the high demand derivatives BaCOa and BaCh and lower volume, val ue-added BaSO4 , BaO, BaCh, Ba(NO2h, BaTiO 3 , barium stearates and barium ferrites. Based on an overview of the market potential for these barium chemicals in Canada and the North-Eastern United States, it was decided to concentrate on the production of commercial quantities of BaS, pri marily for captive use, BaCOs, primarily for sales, BaCh, BaSO4, BaO and Ba(OH)2. Production of these barium chemicals in dedicated production facilities was considered to be the prime criterion although pro duction in a multi-purpose plant was explored as a means of reducing overall production costs. The use of a multi-purpose plant offers the potential of pro ducing additional low volume, value-added, barium chemicals to take advantage of short term market opportunities. In all cases, processing options were selected to take advantage of the best available technology, includ ing established and emerging technologies, to protect the environment by controlling harmful emissions and, if possible, to produce competitively priced final prod ucts. In particular, processes were selected to control sulphur emissions by the production of by-product NaaS, a potentially valuable chemical in the pulp and paper industry. Figure 4 depicts the various processing routes avail able to produce the various barium chemicals from barite/barium sulphide (Ullman et al. 1985) and high lights the routes selected for this study. Production rates for the barium chemicals were established (Table 19) based on the potentially avail able Canadian and North-Eastera United States markets and the need to construct and operate a reasonably sized facility in order to produce competitively priced products. A total of 30,000 tonnes per year of barite concen trate (949fc BaSO4) was assumed to be available from the mineral production facilities. 41 Figure 4. Production Pathways to Various Barium Compounds. Barium Sulphide Barium sulphide, the precursor of most barium chemicals, is produced from high quality barite (min imum 949fc BaSO4) by reduction with a source of carbon. The primary chemical reaction is: BaSO4 + 4C *- BaS + 4CO The most popular process for the production of BaS is the rotary kiln process (Kirk et al. 1984; McKetta Table 19 Production rates for barium chemicals BaS BaCOs (sales) 20,000 tonnes per year 12,000 average, 14,000 maximum BaCI 2 3,500 average, 5,000 maximum BaSO4 1,000 average 1,500 maximum BaO7Ba(OH) 2 (as BaO) 1.500 average, 3,000 maximum 42 and Cunningham 1976; Ullman and Gerhatz 1988; White 1949) in which the reduction reaction is carried out with coal or coke as the source of carbon in a sup plemental fired rotary kiln at temperatures of 1000 to 1250 0 C. Purity of the barite ore must be high, with minimum iron and silicon concentrations, as these impurities tend to form insoluble barium compounds during the reduction process. A crude BaS (black ash), typically containing 75 to 909fc BaS, is discharged from the rotary kiln. Off-gases from the kiln contain particulates and SOz from the sulphur in the coal or coke used in the reduction reaction, from the kiln fuel and from side reactions that occur in the kiln. As a result, removal of particulates and SOz scrubbing are required to avoid air pollution problems and to meet applicable envi ronmental emission standards. Barite reduction to BaS with natural gas in fluidized bed reactors has been discussed in the literature (Kirk et al. 1984; Ullman and Gerhatz 1985) and is report edly being carried out in the U.S.S.R. The fluidized bed process offers several advantages, including lower SOz emissions and the potential for the elimination of the scrubbing systems as the sulphur content of the carbon source and fuel is essentially zero. Addition ally, the purity of the black ash product is potentially higher and lower grades of barite ore can be consid- Barite and Fluorspar in Ontario Table 20 Black Ash Analysis Water Soluble BaS Insoluble Barium Compounds Inert Ash, SiO2, 75-90 0Xo 5-170Xo S-8% ered as no inert materials enter with the carbon source. However, insufficient data were identified to permit an evaluation of the economic feasibility of the process, compared to that of the rotary kiln process. Black ash from either process is a grey/black pow der that reacts readily with moisture and CCh in the air to release H2S. Some black ash is packaged and sold to producers of barium chemicals but most is pro cessed directly into other barium chemicals. The typical analysis for black ash is shown in Table 20. Black ash produced in the kiln for further process ing is wet or dry ground to a fine powder and contacted with water in a series of leaching tanks. The BaS is extracted into the water, forming a 25 to 30^o solution of BaS. The aqueous solution is stored for further pro cessing into other barium chemicals. The undissolved residue or sludge, containing BaCOs and other acid-soluble barium salts, uncon verted BaSO4 and inert impurities, is temporarily stored for further processing into BaCh. Discarding this sludge would reduce the overall yield of barium chemicals from the barite concentrate by 5 to 159fc. The rotary kiln process was selected for use in this study as it represents the established technology and insufficient data were available to permit a valid eval uation of the fluidized bed process. A simplified flow plan for the production of barium sulphide from barite ore via the rotary kiln process is presented in Figure 5 and overall operating parameters are provided in Table 21. The plant is designed to produce 4,400 tonnes per year (as BaS) of black ash for sale, 12,750 tonnes per year (as BaS) of solution for use in the production of BaCO3 and BaSCU and 2,850 tonnes per year (as BaS) of sludge plus BaS solution for use in the production of BaCh. Flexibility is included in the design of the black ash leaching circuit to permit the increased pro duction of BaS solution as the demand for derivative chemicals increases. Barium Carbonate Barium carbonate is the most important derivative of BaS. It is used widely in the manufacture of glass, brick and porcelain, in the electronics industry and as a raw material in the manufacture of specialty barium chemical products. Barium carbonate is precipitated from a solution Table 21 Operating Parameters Barium Sulphide Production PLANT CAPACITY: 20,000 t/a BaS RAW MATERIALS: Barite (940X0 BaSO4) Coal UTILITIES: Natural Gas Electricity PRODUCTS: Black Ash (as BaS), sales BaS Solution (as BaS), captive use BaS Sludge (as BaS), captive use OPERATION: STAFFING: 30,000 t/a 7,500 t/a 7,000 120 kW 4,400 t/a 12,7501/3 2,850 t/a 24 h/d 330 d/y Operations, Maintenance and Administration Options for Barium Chemicals Production 20 43 n C o *- o•3 -o o CL (D CO E D CO Sif c D Q. O LJ- T: o l^ Q. E CO 44 Barite and Fluorspar in Ontario of BaS by the addition of CO2 or NaiCOa (Faith et al. 1975; Kirk et al. 1984; McKetta and Cunningham 1976; Sittig 1968; Ullman and Gerhatz 1985; White 1949). The overall chemical reactions are: BaS * CO2 + H2O *- BaCOs * H2S BaS * Na2CO3 ^ BaCO3 * Na2S The choice between the two processes depends on the availability and cost of the raw materials, CO2 and Na2COs, the desired purity and properties of the prod uct BaCCh and the desired by-product, H2S or Na2S. Carbon dioxide may be recovered from off-gases exiting the BaS kiln or from the exhaust gases of a boiler or fired heater for use in the production of bar ium carbonate. The CO2 is bubbled through the BaS solution to precipitate BaCOs and yield by-product H2S. The BaCOs is recovered by filtration, dried and ground to the desired particle size range. Barium car bonate produced by the CO2 process is a free-flowing powder but typically contains elemental sulphur, BaS and BaSC*4 contaminants. Hydrogen sulphide, generated as a by-product in the CO2 process, must be processed further as it can not be discharged to the atmosphere as H2S or as SO2 for environmental and worker safety reasons. It may be converted to elemental sulphur by the Claus process or to Na2S or (NH4) 2S by reaction with NaOH or NH4OH. All of these processes add to the complexi ty and cost of the production facility but do result in the production of a readily saleable by-product. In the Na2COs process, Na2COa (soda ash) is dis solved in water and reacted with BaS solution to precipitate sulphur-free BaCOs and yield by-product Na2SO4. The barium carbonate is recovered by filtra tion or centrifugation, dried and ground to the desired particle size range. Barium carbonate produced by the Na2CO3 process contains fewer impurities than mate rial produced by the CO2 process as it is free of elemental sulphur and contains very little sulphide or sulphate. Typical product purities are given in Table 22. Barium carbonate produced from Na2COs tends to cake and is not as free-flowing as material produced via the CO2 process. This can be overcome, to a great extent, by the proper selection of drying equipment and conditions. Sodium sulphide is recovered from the reaction solution, after removal of the precipitated BaCOs, by evaporation and crystallization. The Na2S product is recovered as Na2S 3H2O (609fc Na2S) by convention al centrifugation and drying. The Na2COs process was selected for use in this study as Na2COs is readily available in the province, as a high purity BaCOs product is desired and as a potential market exists in the province for by-product Options for Barium Chemicals Production Table 22 Typical Barium Carbonate Purity HCI Insolubles 98.5 0Xo, minimum 0.02-0.080Xo Q.1-0.6% Na2S as a replacement for Na2SCM in Kraft process pulp and paper mills. Additionally, the Na2CO3 process is technically simpler than the CO2 process and capi tal costs are comparable, particularly when recovery facilities for by-product H2S are included. A simplified flow plan for the production of BaCOs from BaS solution and Na2COs is presented in Fig ure 6 and overall operating parameters are provided in Table 23. The plant is designed to produce a maxi mum of 16,000 tonnes per year of BaCOs although the normal operating production will be 13,950 tonnes per year, 12,000 tonnes per year for sale and 1,950 tonnes per year for use in the production of BaCVBa(OH)2. Barium Chloride Barium chloride is used extensively in the elec trolytic production of chlorine and sodium hydroxide, magnesium metal and sodium metal, as a flux in the steel industry and nationally in the uranium industry to precipitate radium. It is also used as a raw materi al in the production of low volume specialty barium chemicals. Barium chloride is produced by reading a barium salt, usually BaS or BaCO3 , with HCI (Kirk et al. 1984; McKetta and Cunningham 1976; Ullman and Gerhatz 1985; White 1949), according to the overall chemical reactions: BaS + 2HC1 *- BaCl2 * H2S BaCO3 + 2HC1 *- BaCl2 * CO2 + H2O The selection of the preferable raw material, BaS or BaCOs, is dependent on their relative availability and cost, the desired purity of the BaCl2 and disposal costs for the by-product H2S in the BaS process. Technical grade BaCl2 (999fc BaCh, minimum, or equivalent in the dihydrate form) is typically produced from BaS sludge and BaS solution from a rotary kiln BaS processing plant. The sludge typically contains 5 to 15*^ of the original barite (BaSCu ) in an acid sol uble form. This can be recovered as technical grade BaCl2 by contacting the sludge with HCI in an agitated reactor and removing Ca, Mg, Al and Si impurities by selective filtration, evaporation and crystallization. High purity grade BaCl2 (99.99fc BaCl2, minimum) 45 BARIUM CARBONATE SODIUM SULPHIDE Figure 6. Simplified Flow Plan for Barium Carbonate Production. is typically produced from BaCOa as a higher purity, but more expensive, raw material. The BaS route to BaCh, making use of the BaS sludge formed in the rotary kiln process for production of the BaS plus additional BaS solution, was selected for use in this study as its use improves the overall uti lization of the barite ore, improves overall economics of the BaS production step and is capable of produc ing technical grade BaCb. A simplified flow plan for the production of BaCh from BaS sludge and HC1 is Table 23 Operating Parameters Barium Carbonate Production PLANT CAPACITY: 16,000 t/a BaCO3 (13,950 t/a normal operation) RAW MATERIALS: BaS Solution (as BaS) UTILITIES: Natural Gas Electricity PRODUCTS: BaCOs, sales BaCOs, captive use Na2S (as Na2 S), sales OPERATION: STAFFING: 46 12,000 t/a 7,500 t/a 10,000 m 37d 200 kW 12,0001/3 1.950 t/a 5,500 t/a 24 h/d 330 d/a Operations, Maintenance and Administration 17 Barite and Fluorspar in Ontario Figure 7. Simplified Flow Plan for Barium Chloride Production, presented in Figure 7 and overall operating parameters are provided in Table 24. The BaCl2 is recovered from solution by vacuum crystallization of BaCl2 -2H2O, filtration and drying. Anhydrous BaCh can be recovered by high tempera ture drying or calcination of the dihydrate. By-product H2S is contacted with NaOH in an agi tated reaction vessel to produce Na2S, according to the overall reaction: H2S + 2NaOH ^ Na2S + 2H 2O The Na2S solution is combined with a similar solu tion from the BaCOs production plant, evaporated and crystallized for recovery of the Na2S. Hydrochloric acid and BaCl2 solutions are very cor- Table 24 Operating Parameters Barium Chloride Production PLANT CAPACITY: 5,000 t/a BaCI 2 (3,500 t/a normal operation) RAW MATERIALS: BaS Sludge (as BaS) HCI (32 0Xo) NaOH (500Xo) UTILITIES: Natural Gas Electricity PRODUCTS: BaCI 2 (as BaCI 2), sales As BaCI 2 -2H 2O Na2S (as Na2S), sales OPERATION: STAFFING: 2,850 t/a 3,850 t/a 2,700 t/a 7,000 rr^/d 120 kW 3,500 t/a 4,1001/3 1,300 t/a 24 h/d 330 d/a Operations, Maintenance and Administration Options for Barium Chemicals Production 12 47 rosive to most common materials of construction and special precautions must be taken in the selection of appropriate materials for equipment components and piping. Fibreglass, graphite, hastelloy, titanium, rub ber-lined steel or plastic-coated steel vessels and components have been successfully used in these or similar applications. Barium Sulphate Synthetic BaSO4, or precipitated BaSO4, is used in applications in which natural barite is not satisfactory. It is used as a filler and extender in rubber and plastic materials and as a paper coating and filler. Important properties are its insolubility in water and organic binders, its high degree of whiteness, its fine grain size and a low iron content. Special photographic and X-ray applications require ultra-high purity BaSCU with less than 10 ppm iron and very low sulphur content. Precipitated BaSO/t, or blanc fixe, for use as a filler and extender is usually manufactured from BaS solu tion by the addition of Na2SO4 (Kirk et al. 1984; McKetta and Cunningham 1976; Ullman and Gerhatz 1985), as per the overall reaction: BaS * Na2SO4 *- BaSO4 + Na2S Special high purity grades of BaSO4 are typically produced from BaCCb or BaCl2 by the addition of Na2SO4 or H2SO4. The production of precipitated BaSO4 from BaS solution via the Na2SO4 route was selected for this study as this grade of product, blanc fixe, represents the greatest share of the potential market, as Na2SO4 is readily available and as Na2S recovery facilities are included in the BaCOa processing plant. A simplified flow plan for the production of BaSO4 from BaS solu tion and Na2SO4 is presented in Figure 8 and overall operating parameters are provided in Table 25. Barium sulphate is produced by contacting BaS solution with high purity Na2SO4 solution in an appro priate reaction vessel. The BaSO4 is recovered by filtration, drying, sintering and grinding to give the desired grain size. The Na2S solution is combined with other solution from the BaCOs and BaCh plants, evaporated and crystallized for recovery of the Na2S. Barium Oxide/Hydroxide Barium oxide and hydroxide are used mainly in the manufacture of oil and grease additives, as the raw material for organic barium salts and for dehydration/deacidification of fats, oils and waxes. Barium oxide is produced primarily by the decom position of BaCOa in the presence of a source of carbon at high temperature (Kirk et al. 1984; McKetta and Cunningham 1976; Sittig 1968). The overall reac tion is: BaCO3 + C —*- BaO + 2CO The use of carbon in the process significantly low ers the temperature at which the BaCOa decomposes; it also serves as a source of energy for the high tem perature process. The decomposition reaction can be carried out in a rotary kiln or in a fluidized bed. In the rotary kiln process, coal, coke or carbon black is used as the source of carbon. As a result, the level of impurities in the carbon source must be carefully controlled to avoid contamination of the BaO product. Most mod ern plants use the fluidized bed process as natural gas can be used as the source of carbon. This results in the production of high purity BaO with typical purity as shown in Table 26. The fluidized bed process was selected for use in this study as it represents state-of-the-art technology Figure 8. Simplified Flow Plan for Barium Sulphate Production. 48 Barite and Fluorspar in Ontario Table 25 Operating Parameters Barium Sulphate Production PLANT CAPACITY: 1,500 t/a BaSO4 (1,000 t/a normal operation) RAW MATERIALS: BaS Solution (as BaS) N32SO4 UTILITIES: Natural Gas Electricity PRODUCTS: BaSCU, sales (as Na2S), sales 2,000 m 37d 100 kW Operations, Maintenance and Administration and produces a high grade, highly reactive product. A simplified flow plan for the fluidized bed process is presented in Figure 9 and overall operating parameters are provided in Table 27. In the fluidized bed process, BaCO3 is contacted with natural gas in the reaction zone at 1000 to 12500C. The BaCO3 decomposes, yielding BaO. The BaO is cooled, ground and packaged for sale. Handling and storage of BaO must be carried out with extreme cau tion and under controlled conditions as the oxide will react with COi and water in the atmosphere to form BaCO3 or Ba(OH)2 in a very exothermic reaction. Much of the BaO produced is converted to more stable Ba(OH)2 products, either the monohydrate or the octahydrate form. Barium hydroxide octahydrate is prepared by adding water to BaO in an appropriate reaction vessel with suitable heat removal capability. The octahydrate product is cooled, flaked and pack aged. Barium hydroxide monohydrate is produced by drying the octahydrate reaction mass in heated vacu um or rotary drum dryers. Multi-Purpose Plant Possibilities The production of barium chemicals from barite or BaS is characterized by reaction between BaS and a Table 26 Purity of Barium Oxide BaO BaCOs BaO2 (peroxide) 1.000 t/a 330 t/a 24 h/d 330 d/a OPERATION: STAFFING: 750 t/a 610 t/a 97-9907o 1-30Xo maximum Options for Barium Chemicals Production number of inorganic salts or acids to produce the bar ium salts, as illustrated below: BaS * Na2CO3 ^ BaCO3 BaS 4- Na2SO4 ^ BaSO4 BaS * 2HC1 *- BaCl2 4- H2S BaS + 2HNO3 * Ba(NO3)2 H2S Many of the reaction systems, product characteris tics and by- product handling requirements are similar, leading to the possibility of constructing a multi-pur pose plant with the capability of producing multiple products in a single production train. Based on an analysis of the processing steps required to produce the selected barium chemicals, BaS, BaCO3 , BaCl 2 , BaSO4 , BaO and Ba(OH) 2 , it appears that the only products that can be produced in a single production train, in blocked operation, are BaCO3 and BaSO4. Production of both barium chem icals involves the reaction of BaS solution with the corresponding sodium salt, Na2CO3 or Na2SO4, result ing in the precipitation of the barium salt and the co-production of by-product Na2S. The barium salt is recovered by filtration or centrifugation, and drying. The Na2S is recovered by evaporation of the solution, crystallization of the Na2S in the trihydrate form, centrifusion and drying. The processing steps required for the production of BaS from barite ore include a high temperature rotary kiln step for the reduction of barite, grinding of the crude BaS or black ash and leaching of soluble BaS from the black ash in a multi-stage leach circuit. These processing steps are different than those used in the production of any of the barium chemicals, with the possible exception of BaO, thereby minimizing the 49 MONOHYDRATE Figure 9. Simplified Flow Plant for Barium Oxide and Barium Hydroxide Production. possibility of their use in producing multiple products. Production of BaCb from BaS and HC1 involves the production of a soluble BaCh and by-product HzS. Recovery of the BaCh from solution involves evapo ration, filtration, vacuum crystallization, product filtration and drying. These processing steps are dif ferent than those used in the production of the other barium chemicals. In addition, HC1 and BaCh are extremely corrosive, requiring special materials of construction for all equipment and piping in contact with them. Finally, conversion of the by-product HiS to saleable NazS requires an additional conversion step, reaction with NaOH. All of these factors mini mize the potential for the production of multiple products which include BaCh in a single plant. Barium oxide is produced in a high temperature rotary kiln or fluidized bed reactor by the reduction of in the presence of carbon. While the process- Table 27 Operating Parameters Barium/Hydroxide Production PLANT CAPACITY: 3,000 t/a BaO (1,500 t/a normal operation) RAW MATERIALS: Barium Carbonate 1,950 t/a UTILITIES: Natural Gas Electricity 800 m 37d 120 kW PRODUCTS: Barium Oxide Barium Hydroxide Octahydrate Barium Hydroxide Monohydrate 500 t/a 1,030 t/a 620 t/a 24 h/d 330 d/a OPERATION: STAFFING: 50 Operations, Maintenance and Administration 12 Barite and Fluorspar in Ontario ing steps appear to be similar to those used in the pro duction of BaS (black ash), the production of both products in a single rotary kiln plant was not consid ered practical because of the concern of contamination of the BaO with residual BaS or barite ore. If the fluidized bed process for the production of BaS from barite ore and natural gas can be shown to be com mercially demonstrated and competitive, the co-production of BaS and BaO in a common plant might be possible as contamination concerns would be minimized. Even though the potential for the production of multiple barium chemicals in a single process unit was found to be limited and only applicable to barium carbonate and barium sulphate, a production complex capable of producing BaS, BaCOs/BaSCU, BaCh and BaCVBa(OH)2 would have a great deal of flexibility for the production of other specialty chemicals to meet low volume, value-added opportunities: * the production of Ba(NO3)2 from BaSO4 and HNO3 * the production of high purity BaCh, BaSO4 or Ba(NOs)2 from BaCOa and the appropriate sodium salt or inorganic acid * the production of lithopone, a white pigment containing BaSO4 and ZnS, from BaS solution and ZnSO4 * the production of barium peroxide by the con trolled heating of BaO in an air/oxygen atmosphere. Production Costs The production costs for the barium chemicals under consideration are dependent on the capital cost of the facilities, the cost of raw materials, the plant operat ing costs, the financial parameters assumed for recovery of invested capital, product marketing costs and the capacity of the production facilities. Preliminary capital cost estimates were prepared for each production facility discussed in the previous section of this report, as presented in Table 28. The capital costs are considered preliminary esti mates as they were factored from budget prices for individual items of process equipment using estab lished estimating procedures. The proposed barium chemicals facility is a stand-alone, grass-roots facil ity with raw materials unloading and storage facilities, process facilities to produce the listed chemicals in dedicated process units, product storage, packaging and loadout systems and all offsite/utility systems needed to operate the facility. A single evapora tion/crystallization unit is provided to recover by-product sodium sulphate from the BaCOs, BaCh and BaSO4 operations. The costs of all common facil ities have been apportioned to the individual production units on the basis of the requirements of each unit so that production costs could be determined for the individual barium chemicals. Preliminary information on the sizes or design capacities of major items of equipment and typical purchase costs are provided in Appendix B. Preliminary production cost estimates were deter mined for each of the barium chemicals under consideration, as summarized in Table 29A. The production cost of each chemical includes the cost of raw materials, the cost of plant utilities, oper ating and maintenance costs, local taxes and insurance, a capital recovery charge of 209fc per year of initial capital cost less by-product credits where applicable. The above production costs are based on a cost of barite, delivered to the chemicals plant, of S108 per tonne. This is considered to be optimistic as the entire 30,000 tonnes per year of barite would have to be pro duced in a single barite production plant in the Thunder Bay area. Established barite reserves in the area may not be adequate to provide sufficient ore for the pro duction of 30,000 tonnes per year of high quality barite Table 28 Estimated Capital Cost for Different Barium Chemical Production Units Chemical Plant Capacity Estimated Production Unit t/a Capital Cost,Smillion BaS BaCO3 BaCI 2 BaSO4 BaO TOTAL FACILITY Options for Barium Chemicals Production 20,000 16,000 5,000 1,500 3,000 11 7 4.8 1.6 4.6 29 51 Table 29A Preliminary Production Costs for Different Barium Chemicals Chemical BaS BaCOs BaCI 2 BaSO4 - dedicated plant - multi-product plant BaO Ba(OH) 2 - Monohydrate - Octahydrate Normal Production t/a Production Cost, S/t 413 388 592 567 1,098 4,400 15,600 12,000 1,950 3,500 sales captive sales captive sales Reported Market ValueS/t N/A 550-800 500-840 1,000 1,000 1,085 sales 815 sales 800 800 500 1,890 sales N/A 620 1,030 1,535 sales 920 sales 1100-1250 N/A BaSO4 , minimum). The barium chemicals plant would be located in Thunder Bay in this case to min imize shipping costs for the barite. A more realistic case to consider is the use of barite recovered from Hemlo gold mill tailings or barite min erals produced at two 15,000 tonnes per year production plants, one in the Thunder Bay area and one in the Matachewan area, for the production of the bar ium chemicals. The barium chemicals plant, in this case, would be centrally located to be closer to the barium chemicals market, thereby necessitating ship ment of the barite from the production plants to the chemicals plant. The estimated production and ship ping cost for barite is in the range of S180 to 3210 per tonne. With this higher cost feedstock, the production cost of the barium chemicals increases proportional ly, illustrated in Table 29B. All new equipment was assumed in preparing cap ital cost estimates for the barium chemicals facility. For certain items of equipment, in particular the rotary kiln in the BaS plant, product filters, centrifuges, dry ers and grinding mills, the potential exists for utilizing used, reconditioned equipment, thereby reducing the capital cost of the production facilities. Selective use of reconditioned equipment throughout the chemicals facility would reduce the overall capital cost by only 5 to 109fc as direct equipment costs only contribute 25 to 30^o of the total cost of a typical chemicals project. A reduction in capital cost of this magnitude would not dramatically affect the production cost of the bar ium chemicals as capital-related costs only make up a portion of the estimated production costs. Indicated production costs would only be reduced 2 to 39fc as a result of the selective use of reconditioned equipment. Table 29B Production Costs for Barium Chemicals Using Higher Cost Feed Stock Chemical BaS (captive) BaCOs (sales) BaCI 2 BaSO4 - dedicated plant - multi-product plant BaO Ba(OH) 2 - Monohydrate - Octahydrate 52 Plant Gate Production Cost, S/t Barite @ S108/t Barite @ S180-210/t 388 592 1,098 495-540 685-725 1,185-1,220 1,165-1,200 1,085 815 1,890 895-930 2,010-2,060 1,535 920 1,635-1,675 980-1,000 Barite and Fluorspar in Ontario Basis for Capital and Production Cost Estimates Preliminary capital cost estimates were developed for each barium chemical production unit (BaS, BaCOs, BaCh, BaSO4 and BaO7Ba(OH)2), as part of a grass roots barium chemicals production complex. Each barium chemical is produced in a dedicated production unit with dedicated raw materials storage and product storage facilities. Common support facilities are pro vided for the chemicals complex. These include raw materials unloading systems, product packaging and loadout systems, offsite and utility systems needed to operate the facility and effluent treatment/environmental control systems. In addition, a single evaporation/crys tallization unit is provided to recover by-product NaaS for sale from the BaCOa, BaCh and BaSCu operations. The cost of all common facilities have been appor tioned to the individual production units on the basis of the requirements of each unit so that production costs can be determined for the individual barium chemicals. The estimated capital costs were based on budget prices for major items of process equipment plus fac tors for installation, piping, instrumentation, electrics, structural steel and concrete, site services, process buildings, engineering and construction, spare parts and startup allowances and overall project contingen cies, using established estimating procedures. No allowances were included for land acquisition, for major warehousing of raw materials or final products or for environmental assessment costs. The production cost estimate for each barium chem ical includes the cost of raw materials, the cost of plant utilities (natural gas, electricity, water), operat ing and maintenance costs (labour, replacement parts, supplies), local taxes and insurance, a capital recov ery charge of 209fc per year of initial capital cost, less by-product credits where applicable. Table 30 shows the main cost parameters used in determining the pro duction cost for each barium chemical. A capital recovery factor of 209fc per year was selected as it represents the minimum return on capi- Table 30 Main Cost Parameters Used in Determining Production for Barium Chemicals RAW MATERIALS Barite Na2CO3 Sl087t, base price, single mill (S1 80-21 0/t from alternate sources, Hemlo or two smaller processing mills) S225A N32SO4 HCI (32 0Xo) NaOH (50 0Xo) Coal (low sulphur) UTILITIES Natural Gas Electricity Treated Water S 80/t S1 20/1 03m 3 SO.OS/kWh Operations and Administration Staff Manpower count for each plant, S40,0007annum average Maintenance Parts and Labour 40Xo of capital cost/yr Taxes and Insurance 1 0Xo of capital cost/yr Operating Supplies 100Xo nominal of the cost of utilities, labour and maintenance Capital Recovery Charge 20pXo of capital cost/yr By-Product Credit S2507t to be marketed primarily to pulp and paper companies as a replacement for sodium sulphate in Kraft mills. Marketing Cost An allowance of S257t of net saleable product. Options for Barium Chemicals Production 53 Table 31 Production Cost Summary Barium Sulphide PLANT CAPACITY: 20,000 tonnes per year BaS CAPITAL COST: S11.000,000 PRODUCTION COST ANNUAL COST, UNIT COST, S S/t BaS Raw Materials- Barite - Coal 3,240,000. 600,000. 162.00 30.00 Utilities- Natural Gas - Electricity - Water Operations and Administration Staff Maintenance Labour and Parts Taxes and Insurance Operating Supplies Capital Recovery 277,000. 48,000. 66,000. 640,000. 442,000. 110,000. 137,000. 2,200,000. 13.85 2.40 3.30 32.00 22.10 5.50 6.85 110.00 Total Production Cost 7,760,000. 388.00 Marketing Cost (for net sales) 25.00 Plant Gate Price tal expected by a private investor. A capital recovery factor of 209fc, or a simple payback of 5.0 years, equates approximately to an after-tax discounted cash flow return on investment of 15*^, in constant dollars. The estimated production costs do not include prod uct shipping costs to potential customers, dealer markups or the impact of the Goods and Services Tax. Market prices for barium chemicals discussed in this section of the report, as an indication of the eco nomic potential for the production of individual materials, were taken from the Law, Sigurdson & Asso ciates and SRI International report (1989). Barium Sulphide The estimated capital cost of the BaS plant, with a production capacity of 20,000 tonnes per year of BaS (as BaS), is Sil million. The estimated production cost of BaS, with a base barite price of S108 per tonne, is S388 per tonne for captive use material and S413 per tonne for net sales product, as presented in Table 31. In order to realize the S108 per tonne production and delivery cost for barite, a single mineral processing mill with a capacity of 30,000 tonnes per year of high quality barite would be required. Both the processing mill and the chemicals production facility would have to be located in the Thunder Bay area, close to estab 54 413.00 lished mineral deposits, to minimize barite trans portation costs. Processing of higher cost barite, such as barite recovered from Hemlo area gold mill tailings or barite produced in two smaller processing mills (15,000 tonnes per year mills at Thunder Bay and Matachewan) and shipped to a central chemicals facility, would result in higher cost barium sulphite, as shown in Table 32. Although market values are not reported regularly for BaS, primarily as the bulk of the material is for cap tive use, it is believed that the indicated production cost of S388 to 413 per tonne (with S108 per tonne barite) is competitive with current supplies. The major consideration, however, is the impact of this BaS cost Table 32 Barium Sulphide Production Cost Barite @ Sl087t S3887t captive use S413/1 sales Barite @ S180-210/t S495-5407t captive use S520-5657t sales Barite and Fluorspar in Ontario Table 33 Production Cost Summary Barium Carbonate PLANT CAPACITY: 16,000 t/a BaCO3 (13,950 t/a normal operation) CAPITAL COST: S7,000,000 PRODUCTION COST ANNUAL COST, S UNIT COST, S/t BaCOs Raw Materials- BaS Solution - Sodium Carbonate 4,656,000. 1,688,000. 333.76 121.00 Utilities- Natural Gas - Electricity - Water Operations and Administration Staff Maintenance Labour and Parts Taxes and Insurance Operating Supplies Capital Recovery 396,000. 79,000. 20,000. 560,000. 281,000. 70,000. 135,000. 1,400,000. 28.38 5.66 1.43 40.14 20.14 5.02 9.68 100.36 Total Production Cost 9,285,000. 665.57 (1,375,000.) (98.57) 7,910,000. 567.00 By-Product Na2S Credit Net Production Cost Marketing cost (for net sales) 25.00 Plant Gate Price on the production cost of the other barium chemicals as BaS is the precursor of these materials. Net sales of BaS are assumed to be only 4,400 tonnes per year; this quantity would probably be reduced as the demand for other value-added barium chemicals increases. Barium Carbonate The estimated capital cost for the BaCOs plant, with a production capacity of 16,000 tonnes per year of BaCOs, is S7 million. The estimated production cost of BaCOs is S567 per tonne for captive use mate rial and S592 per tonne for net sales product, relative to the base barite price of 5108 per tonne, as present ed in Table 33. This price increases substantially as the price of barite ore increases to the range of S180 to 210 per tonne, as shown in Table 34. Normal operating capacity in the BaCOs plant is assumed to be 13,950 tonnes per year of BaCCh, 12,000 tonnes per year for sales and 1,950 tonnes per year for captive use in the production of BaO and Ba(OH)2 . Market values for BaCOa are reported to be in the Options for Barium Chemicals Production 592.00 range of S550 to S800 Cdn per tonne for high grade material supplied in Canada and the North-Eastern United States, with Chinese material costing S550 to S600 per tonne and European product costing S800 per tonne. U.S. quoted list prices are in the range of S740 Cdn per tonne, FOB plant in Georgia. Based on this information, there appears to be an economic potential for the production of BaCOa and the precursor BaS in Ontario for marketing in Cana da and the North-Eastern United States provided that competitive barite ore prices (below about S120 to Table 34 Barium Carbonate Production Cost Barite @ S1087I (BaS @ S3887t) S5677t captive use S5927t sales Barite @ S180-2107t (BaS @ S495-5407t) S660-7007t captive use S685-7257t sales 55 Table 35 Production Cost Summary Barium Chloride PLANT CAPACITY: CAPITAL COST: 5,000 T/A BAC1 2 (3,500 t/a normal operation) S4,800,000 PRODUCTION COST Raw Materials- BaS Sludge - Hydrochloric Acid - Sodium Hydroxide Utilities- Natural Gas - Electricity - Water Operations and Administration Staff Maintenance Labour and Parts Taxes and Insurance Operating Supplies Capital Recovery Total Production Cost By-Product Na2S Credit Net Production Cost Marketing Cost Plant Gate Price - as Barium Chloride - as Barium Chloride Dihydrate S150 per tonne), delivered to the chemicals plant, can be realized. A production facility capable of produc ing 15,000 to 20,000 tonnes per year of barium sulphide (6,000 to 8,000 tonnes per year net sales) and 10,000 to 15,000 tonnes per year of barium car bonate is considered to be an economic size. Unit production costs increase rapidly in smaller sized plants as capital recovery charges and fixed operating costs remain relatively constant, representing an ever increasing portion of the unit production cost as plant production rate is reduced. ANNUAL COST, S UNIT COST, S/t BaCh 1,106,000. 674,000. 405,000. 316.00 192.57 115.72 158,000. 48,000. 5,000. 400,000. 45.14 13.72 1.43 960,000. 114.29 54.86 13.72 24.13 274.27 4,080,500. 1,165.85 192,000. 48,000. 84,500. (92.85) (325,000.) 3,755,000. 1,073.00 25.00 1,098.00 937.00 Barium Chloride The estimated capital cost for the BaCh plant, with a production capacity of 5,000 tonnes per year of BaCh, is S4.8 million. The estimated production cost for BaCh, for a normal operating capacity of 3,500 tonnes per year, is presented in Table 35. An overall production cost (or plant gate price) of S l,098 per tonne for anhydrous barium chloride or S937 per tonne for BaCh-2H2O is indicated, relative to the base barite price of S108 per tonne. These prices increase mod erately as the price of barite increases to the range of S180 to S210 per tonne, as presented in Table 36. Table 36 Barium Chloride Production Cost Barite @ (BaS @ S388A) Barite @ S180-210/t (BaS @ S495-5407t) 56 Anhydrous Dihydrate Sl,0987t S9377t S1,185-1,220A Sl,010-1,0457t Barite and Fluorspar in Ontario Market values for anhydrous BaCh are reported to be in the range of S500 to S840 Cdn per tonne, based largely on product purity. Quoted prices for U.S. and European material, which are high quality product, are at the upper end of this price range, that is, S800 to S840 per tonne. Even if 3800 to S840 per tonne can be realized for BaCh produced in an Ontario based chemical facili ty, it does not appear that its production has any immediate economic potential. Indicated production costs are in the range of S l, 100 per tonne (anhydrous basis) even with optimistically priced barite ore. Barium Sulphate The estimated capital cost of a dedicated BaSO4 plant, with a production capacity of 1,500 tonnes per year of barium sulphate, is S 1.6 million. The estimat ed production cost for barium sulphate in a dedicated plant, for a normal operating capacity of l ,000 tonnes per year, is presented in Table 37. A plant gate pro duction price of 31,085 per tonne is estimated, relative to the base barite price of S108 per tonne. This price increases moderately with increased barite prices. As an option, the co-production of BaCOs and BaSO4 in a single production unit (multi-product plant) was considered as a means of reducing the produc tion cost of the BaSO4. This type of operation appears to be feasible as the processing steps for the produc tion of BaCOs and BaSO4 are similar, with the main difference being in the use of NaiCOa as raw materi al for the production of BaCOa and NazSCU for BaSCU. The estimated capital cost of the BaCCb/ BaSO4 plant, with a combined capacity of 16,000 tonnes per year BaCOa and 1,500 tonnes per year BaSO4, is S8.4 mil lion. The estimated production costs for the BaCOa and BaSO4, for normal operating capacities of 13,950 tonnes per year BaCOa and 1,000 tonnes per year BaSO4, are presented in Table 38. By keeping the pro duction cost for BaCOa the same as in the dedicated plant situation, a plant gate production price for BaSO4 of S815 per tonne is indicated. This is significantly lower than in the dedicated plant case as substantial operating cost savings are realized. Table 37 Production Cost Summary Barium Sulphate PLANT CAPACITY: 1 .500 T/A BASO4 (1,000 t/a normal operation) CAPITAL COST: S1, 600,000 PRODUCTION COST ANNUAL COST, S UNIT COST, S/t BaSO4 Raw Materials- BaS Solution - Sodium Sulphate 291,000 92,000 291.00 92.00 Utilities- Natural Gas 79,000 40,000 3,000 200,000 62,000 16,000 39,000 320,000 79.00 40.00 3.00 200.00 62.00 16.00 39.00 320.00 1,142,000 1,142.00 - Electricity - Water Operations and Administration Staff Maintenance Labour and Parts Taxes and Insurance Operating Supplies Capital Recovery Total Production Cost By-Product NaaS Credit Net Production Cost Marketing Cost Plant Gate Price Options for Barium Chemicals Production (82,000) 1,060,000 (82.00) 1,060.00 25.00 1,085.00 57 Table 38 Production Cost Summary Barium Carbonate and Sulphate in Single Plant PLANT CAPACITY: 16,000 t/a BaCO3 + 1,500 t/a BaSO4 (13,950 t/a and 1,000 t/a normal operation) CAPITAL COST: S8,400,000 PRODUCTION COST ANNUAL COST, BaCOa S ANNUAL COST, BaSO4 S Raw Materials- BaS Solution - Sodium Carbonate - Sodium Sulphate 4,656,000 1,688,000 - 291,000 92,000 Utilities- Natural Gas - Electricity - Water Operations S Administration Staff Maintenance Labour and Parts Taxes and Insurance Operating Supplies Capital Recovery 396,000 79,000 20,000 560,000 281,000 70,000 135,000 1,400,000 79,000 40,000 3,000 55,000 14,000 18,000 280,000 Total Production Cost 9,285,000 872,000 (1,375,000) (82,000) 7,910,000 790,000 By-Product Na2S Credit Net Production Cost Net Production Cost, S/t 567.00 790.00 25.00 25.00 592.00 815.00 Marketing Cost (net sales), S/t Plant Gate Price, S/t Table 39 is a summary of barium sulphate produc tion costs (plant gate price) as a function of barite price. Market values for BaSO4 are reported to be in the range of 5800 Cdn per tonne for synthetic, pigment and filler grade material. Based on this information, it does not appear that there is any significant econom ic potential for the production of BaSO4 in an Ontario-based chemical facility even with optimisti cally priced barite ore. However, production of BaS04 in a multi-product BaCOs plant might be considered to meet short term demands for high quality, value added product. Table 39 Barium Sulphate Production Cost Barite @ (BaS @ SSSS/t) Barite @ Dedicated Plant Multi-Purpose Plant SLOSS/t S895-930A (BaS @ S495-540A) 58 Barite and Fluorspar in Ontario Table 40 Production Cost Summary Barium Oxide/Hydroxide PLANT CAPACITY: 3,000 t/a BaO (1,500 t/a normal operation) CAPITAL COST: S4,600,000 PRODUCTION COST Raw Materials- Barium Carbonate Utilities- Natural Gas - Electricity - Water Operations and Administration Staff Maintenance Labour and Parts Taxes and Insurance Operating Supplies Capital Recovery Total Production Cost Marketing Cost Plant Gate Price - as Barium Oxide - as Barium Hydroxide Monohydrate - as Barium Hydroxide Octahydrate ANNUAL COST, UNIT COST, S S/t BaO 1,105,500. 737.00 32,000. 48,000 3,000. 400,000. 183,000. 46,000. 60,000. 920,000. 21.33 32.00 2.00 266.67 122.00 30.67 40.00 613.33 2,797,500. 1,865.00 25.00 1,890.00 1,535.00 920.00 Barium Oxide/Hydroxide The estimated capital cost for a BaO7Ba(OH)2 plant, with a production capacity of 3,000 tonnes per year of BaO equivalent (BaO plus Ba(OH) 2), is S4.6 million. The estimated production costs for barium oxide and hydroxides, for a normal operating capacity of 1,500 tonnes per year barium oxide equivalent, are present ed in Table 40. Plant gate production prices of S l,890 per tonne for BaO, S l,535 per tonne for Ba(OH)2.H2O and S920 per tonne for Ba(OH) 2 -8H2O are indicated. These prices increase moderately with increased barite prices, as shown in Table 41. Market values for Ba(OH)2-H2O, the highest volume chemical of the BaO7Ba(OH)2 family of chemicals, are reported to be in the range of S l, 100 to 31,200 per tonne for high quality material. As the product cannot be produced economically at this price in an Ontario based chemicals facility, even with opti mistically priced barite, there does not appear to be any significant economic potential for its production. Options for Barium Chemicals Production 59 Table 41 Barium Oxide Production Cost Barite @ SlOS/t (BaCO3 @ S5677t) Barite @ S180-210/t (BaCOa @ S660-7007t) Barium Hydroxide Production Cost Barite @ $108/t (BaCO3 @ Barite @ S1 80-21 0/t (BaCO3 @ S660-7007t) 60 Sl,8907t S2,010-2,060/t Monohydrate Octahydrate S1 ,535/t S9207t S1 ,635-1 ,675/t S980-1 ,000/t Barite and Fluorspar in Ontario 5. Options for Fluorspar Production Options for Fluorspar Production Production Options The North American market for fluorspar includes the metallurgical and acid grade material. Major pro ducers in Canada, the United States and Mexico have a combined production capacity of approximately l .4 million tonnes, reported for 1987 (Prud'homme 1989). Metallurgical grade material, generally above 609fc Ca?2 content, is supplied to steel mills. Acid grade material, with a minimum of 979fc CaFz content, is used mainly for HF production and alumina refining. Total imports to Canada amounted to 194,000 tonnes (all material) in 1988, of which about 70*fo is report ed to be acid grade material (Law, Sigurdson and Associates and SRI International 1989). Most of this is obtained from Mexico although the recently com missioned plant of St. Lawrence Fluorspar in Newfoundland has a capacity of 80,000 tonnes per year. A major consumer in Ontario is the Allied Sig nal plant in Amherstburg. Prud'homme 1989 has noted that the stringent spec ifications for acid grade material have created a slight price increase, and that "Producers of high grade filtercake are in a better position to absorb any fluc tuations in demand." Considering the nature of known fluorspar deposits in Ontario and the volume of imported material, the most favourable production option in Ontario appears to be for acid grade material. Low shipping costs to an Ontario based consumer should outweigh the probably lower production costs of the major suppliers of imported material. The known resources in Ontario preclude consid eration of a large production facility. Based on typical grades of deposits and dispersion of the vein struc tures, a production rate of 15,000 tonnes per year is considered reasonable for initial operation of a cen tralized processing plant. This would entail mining of up to 50,000 tonnes per year of material containing an average of 509fc CaFi. A favourable location would be in South-Eastern Ontario near the town of Madoc. Such a plant would be designed to produce acidgrade fluorspar. Depending on the nature of material mined, barite might also be produced as a by-product. Studies by CANMET with samples of fluorspar from many Canadian locations showed a difficulty in upgrading to acid-grade material (Collings and Andrews 1988b). Gravity separation methods pro duced concentrates often below 90^o CaFi due to the difficulty in separating fluorspar from other minerals having similar characteristics. Flotation tests illus trated the potential of the method for producing the required grade of concentrate. Barite was removed by 61 flotation prior to fluorspar recovery from samples con taining both minerals. A processing plant designed to treat a variety of ores, as mined from several veins, is proposed as a centrally located facility. Processes selected to achieve the maximum possible upgrading, by removal of con taminants, are included. In the proposed mill, fluorspar is crushed and reduced by hammer mill prior to initial recovery by jigs and tables. A high grade gravity concentrate may be produced if the mineralogy of the ore is suitable. Rejects from the gravity circuit are ground to less than 300 |im prior to removal of metal sulphides (pyrite and others) and barite in flotation circuits. A final flotation stage will recover a fluorspar concentrate. Further upgrading of the concentrate will be achieved by high intensity magnetic separation. The concen trate will be filtered and dried for shipment. The flowsheet is illustrated in Figure 10. Specifications Acid Grade Fluorspar The specifications for acid grade fluorspar are set by the consumers and are based on level of contami nants and size analysis. A typical specification is illustrated in Table 42. Material meeting these specifications is generally produced by plants employing flotation, but not all sources can satisfy the restrictions which may be imposed on minor levels of contaminants including lead, phosphorus and arsenic. Metallurgical Grade Fluorspar The specifications for fluorspar sold as metallurgical grade material vary according to the demands of the particular consumers, mainly steel plants. Generally a minimum level for (CaF2) content is 60*26, and size analysis is specified. Reported specifications for three Ontario steel plants (Collings and Andrews 1988b) indicate a higher required level of CaF2 between 75 and 809fc. Specifications for contaminants by these con sumers range as shown in Table 43. Effective CaF2 equals Total CaF2 minus 2.5 times silica content (McKetta and Cunningham 1976). Table 42 Typical Specification for Acid Grade Fluorspar Calcium fluoride Silica Calcium carbonate Sulphur Heavy metal oxides Particle size 970Xo 10/0 1 .2507o o. 030/0 Q.4% 150 minimum maximum maximum maximum maximum (im * *References Collings and Andrews 1988b; Law, Sigurdson and Associates SRI International 1989. Table 43 Typical Specification for Metallurgical Grade Fluorspar Calcium fluoride (Effective) Silica Calcium carbonate Sulphur Lead 75-800/0 2-60/0 2-30/0 0.01-1.00/0 0.02-0.250/0 minimum maximum maximum maximum maximum *References Collings and Andrews 1988b; Law, Sigurdson and Associates SRI International 1989. 62 Barite and fluorspar in Ontario OPEN PIT MINE WASTE ROCK 40-SOX CoF2 i JAW CRUSHER TO 2* CLAY. SUMES LOG WASHER SURGE BIN SIZE REDUCTION (HAMMERMILL) l PRODUCT -1/2' fTJUORITE JIGS CONC. ^ ^ 3 uutlMC TADLTJIAKINC TADLC- v TAILINGS <———————————— 1, FLUORSPAR GRAVITY ^ CONCENTRATE X JL f" ROD MILL TO -300 urn w —300 urn ^———————— PYRITE ROUGHER FLOTN. PYRITE CONC. CONC. CONDITIONER BARITE ROUGHER FLOTN. CONC. ^ BARITE CLEANERS 6 STAGES ' FLUORITE ROUGHER FLOTN. CONC. ——> ; t p 1 f BARITE FLOTATION CONCEN TRATE k FLUORITE CLEANERS 8 STAGES \ f )r )r <————————————————————————————————— \ f FLOTATION TAILINGS ^ ^ ^^ r HIGH INTENSITY MAG. SEPARATION ^ ^ FLUORITE CONC. 4-97X )f REJE:CTS \r cii TDATinjki Aurt novnjn ^FLUORSPAR TO CHEMICAL PLANT Figure 10. Fluorspar Recovery from Vein Mine. Options for Fluorspar Production 63 Size analysis specifications appear to restrict the quantity of fine and coarse fractions. Production Costs S147 per tonne of product. The total production cost including repayment of capital (within five years) is estimated to be S198 per tonne of product. Metallurgical Grade Material Acid Grade Material A proposed fluorspar processing plant would be located centrally to treat ores mined from a number of vein deposits in the Madoc area. The production rate considered is 15,000 tonnes per year of fluorspar con centrate meeting acid grade specifications. The estimated capital cost of the facility is approx imately S3.8 million. Mining costs for development of deposits are not included and it is assumed that min ing on a contract basis, or by owner-operators of small deposits, will supply feed to the plant. Preliminary information on the sizes of major items of equipment and typical purchase costs are provided in Appendix C. A total of 14 personnel are required for plant oper ation and administration, plus contractors engaged in mining and trucking. The estimated production cost is presented in Table 44. The direct operating cost, including mining and ore haulage, is approximately The production of metallurgical grade fluorspar from the known Ontario deposits has not been con sidered in detail due to the small volume and dispersed nature of the deposits, and the limited market poten tial. Metallurgical grade material could be produced by a simple gravity processing plant or as a secondary product from a plant designed to produce acid grade material as a primary concentrate. A very preliminary estimate of capital cost is approximately S2 million for a plant designed to treat the proposed mine output of 46,000 tonnes per year, using gravity recovery only. The direct operating cost would be in the order of S70 per tonne of product (707o CaFi) and the total production cost, including capital repayment, approximately S90 per tonne. Table 44 Mill Production Cost Summary Fluorspar Mill Open Pit Mine ANNUAL COST, S UNIT COST, S/t ore UNIT COST, S/t Product Payroll 582,000 12.65 38.80 Reagents and Supplies 391,000 8.50 26.07 30,000 0.65 2.00 Power and Fuel 171,000 3.72 11.40 Contract Mining 644,000 14.00 42.93 Ore Haulage to Mill 18,400 0.40 1.23 Insurance, taxes etc 50,000 1.09 3.33 General 122,000 2.65 8.13 Contingency 200,840 4.37 13.39 2,209,240 48.03 147.28 760,700 16.54 50.71 2,969,940 64.56 198.00 Maintenance Supplies Direct Operating Cost Capital Repayment Total Production Cost Note: Milling Rate = 46,000 tonnes per year Product Rate = 15,000 tonnes per year 64 Barite and Fluorspar in Ontario 6. Implications for Small Mines Custom Milling The deposits of barite and fluorspar occurring in Ontario are generally small, often narrow vein deposits. The proposed production options for the major deposits are designed on the basis of centrally located pro cessing plants in order to optimize costs and handling of material. The proposed location of the plants would also allow smaller quantities of ore, supplied by inde pendent operators in the immediate area, to be treated on a custom milling basis. Barite A barite processing plant located in the Thunder Bay area could provide a valuable custom milling opportunity. The plant as proposed would be designed to receive ore from several vein deposits in order to satisfy either of the indicated production rates of 15,000 tonnes per year or 30,000 tonnes per year. Since ore from the major deposits will be trucked to the crushing station at the plant, other suppliers could quite feasibly use the same approach. A number of small vein deposits are known to occur within the dis trict and most of them are probably within economic haulage distance of a suitable mill site. The known deposits generally contain a high pro portion of barite and contaminants seem to be fairly constant thus predictable. It is possible that other small deposits worked by independents or owneroperators could supply small portions of the feed to such a mill. Supplies of custom ore could be stockpiled at the mill site to allow a campaign type operation or could be blended with the regular mine production if simi lar in grade. The campaign method is probably better suited to this project where the milling operation is not continuous and payment for custom ore may depend on recovered mineral quantities. For the North-Eastern region of the province the same possibilities exist for custom ore milling except that the distances between some of the noted deposits tend to be greater. The viability of a processing facil ity in this area will in part depend on the availability of ore supply from the existing mining operations. Ore from other known deposits appears to be com patible with the present ore supply and this does present an opportunity to develop small deposits if they are found within an economic haulage radius. The proposed plant for this area is also designed for two shifts per day of operation, five days per week, so it could easily accommodate a fluctuating supply of additional ore, and allow process changes between campaigns. Implications for Small Mines 65 The South-Eastern region could probably benefit from the services of a custom milling operation; it is assumed that some of the available small reserves could be mined by local owners for treatment at a nearby plant. However, justification for such an instal lation requires considerably more work and data collection to develop a regional reserve estimate. Fluorspar The major occurrences of fluorspar are stated to be in South-Eastern Ontario in the vicinity of Madoc, and the proposed fluorspar processing plant is sug gested for this area. This plant would depend on supply of ore from a number of separate vein deposits, prob ably even at the relatively low production rate of 15,000 tonnes per year. While ownership of the deposits has not been researched, it is likely that some of these fall into the category of independent own er/operators. As such, the proposed plant is, in part, a custom mill. The establishment of a plant in the area, designed to treat a variety of deposits, will encourage explo ration and development of other deposits by local owners who could not afford to participate in the ini tial enterprise. As with the barite plant, the design allows for easy expansion of production and cam paigning of separate ore supplies. The processes included also allow rejection and/or recovery of oth er minerals. By-product Recovery Barite at Hemlo The three producing gold mines at Hemlo are min ing ore from underground workings using modern, cost effective techniques. These operations are prof itable due to the gold content of the ore and the large tonnage, efficient operations. In effect, the barite avail able in the tailings of the Hemlo mills is mined at zero cost. Unless there are easily worked, high grade surface deposits of barite in the area, it is doubtful a new or independent operation could produce barite at a similar or lower cost than projected for the proposed tailings treatment plant. It is possible that other gold (or base metal) deposits will be developed in the area, and possibly as small operations. Ore from such potential operations may contain barite, but it is unlikely that the barite content would be considered in establishing the feasibility of a new operation. The operating gold mills are presently running at capacity and there is a low probability that the option of custom milling ore from other sources would be entertained. Fluorspar Within Ontario there is no known current mining operation where an ore is being processed which also contains significant quantities of fluorspar. However, there are mining and milling operations in areas where fluorspar ore could be mined on a small scale (NorthWestern and South-Eastern Ontario). While these existing mills do not have fluorspar recovery circuits installed, it is quite probable that a minor amount of additional equipment could be installed to allow co-processing of a fluorspar sup ply. Such a facility would allow crushing and grinding of the custom ore in parallel operation or on a cam paign basis. The use of either excess flotation capacity or additional flotation equipment for fluorspar pro cessing would then incur a fairly low level of new capital expenditure. The advantage to potential custom shippers would be the available infrastructure, shared labour costs and services of an existing plant. Barite/Fluorspar Joint Recovery The noted vein deposits of the Madoc area and some occurrences in the Thunder Bay area contain both barite and fluorspar. For the Madoc deposits mined in the past, selective mining and/or hand sorting was practised in order to separate the two minerals to a 66 Barite and Fluorspar in Ontario maximum extent prior to processing. Guillet (1963) reported that concentrates of both barite and fluorspar were produced at the Noyes Mine. The fluorspar processing plant proposed earlier in this report includes processes to remove barite prior to recovery of fluorspar. This would be a necessity for a plant in the Madoc area in order to meet acid grade fluorspar specifications. With recent advances in the development of flota tion chemicals, it is conceivable that such a plant could process a variety of ores to produce acceptable barite and fluorspar concentrates. This would be advan tageous to operators of small mines where selective mining is not effective or economic. Plant operation would probably be controlled to either process a fixed blend of ores or to combine ores of widely different barite/fluorspar ratios. This would suit small mine production where production rates might fluctuate on a short term. Implications for Small Mines 67 68 Barite and Fluorspar in Ontario 7, Conclusions and Recommen dations Conclusions and Recommendations Conclusions 1. Development of a plant to produce 30,000 tonnes per year of chemical grade barite appears practical for several areas in the province, based on prelimi nary information concerning resource volumes and grade. The most attractive possibility is a facility located near Thunder Bay, producing barite at an esti mated cost of S108 per tonne. 2. Similar production rates for barite might be achieved by mills at Hemlo or near Matachewan but production costs will be higher. Current operations at these locations may also restrict development or impose added costs. 3. The production of BaS, BaCOa and possibly BaSO4 in a multi-product carbonate/sulphate plant appears to offer reasonable technical and economic potential provided that low cost barite can be delivered to the barium chemicals plant and that the reported market prices for these chemicals are realistic for large volume quantities. Production rates and plant gate production costs for these chemicals, using S108 per tonne barite are shown in Table 45. 4. The production of BaCh, BaO and Ba(OH)2 does not appear to have any significant economic poten tial as indicated production costs are well in excess of reported market prices in Canada and the Eastern Unit ed States even with low price barite. 5. Product transportation costs are significant and siting of the barium chemicals plant relative to the barite milling operation(s), existing transportation sys tems and the barium chemicals marketplace is an important consideration. 6. The most likely area for development of a fluorspar processing facility appears to be in the region near Madoc. Acid grade fluorspar could be produced but the operation may be limited by the available min eral resource. A cost developed for production of 15,000 tonnes per year of acid grade material is S198 per tonne. 7. The most attractive processing options for both barite and fluorspar favour custom milling opportu nities for small mine operators. The fluorspar plant would also allow co-processing of barite-rich ore for the possible production of two concentrates. 8. The costs developed for this study must be con sidered as preliminary. They are based on a minimum level of information concerning mineral deposits, met allurgical testing and processing options. The documents referenced have been relied upon implic itly for all raw data. 69 Table 45 Production Rates and Plant Gate Costs for Barium Sulphide, Barium Carbonate and Barium Sulphate Production Rate, t/a Production Cost, S/t Barium Sulphide - captive use - net sales 15,600 4,400 413 Barium Carbonate 12,000 592 1,000 815 Barium Sulphate Recommendations 1. It is recommended that additional work be con ducted to establish the validity of the most attractive options for barite and fluorspar production. The most critical is the need to establish a base level of proven and probable reserves of the economic minerals. 2. Following investigation of reserves, studies must be conducted to: * Test representative samples of the reserves to develop efficient and cost effective metallur gical processing routes; * Examine potential mine and plant locations in order to define costs of land acquisition, site development, buildings, tailings disposal, infrastructure and supply of services; * Complete a market survey for the minerals being considered; * Conduct feasibility studies for the selected min erals and processing options. * Conduct a detailed feasibility study on pro duction of the selected barium chemicals at production rates determined by the results of the market analysis and the barite mineral avail ability/cost studies. Only after these studies and investigations have been completed can serious consideration be given to proceeding with the development of barite and fluorspar reserves in Ontario and to the consideration of barium chemicals production to take advantage of potential market opportunities in Canada and the East ern United States. 3. Following successful completion of a feasibili ty study to define the processing costs for high quality barite (949fc BaSO4 minimum), chemicals production studies must be conducted to: * Better define the market opportunities for pri mary barium chemicals (sulphide, carbonate and sulphate) in Canada and the Eastern Unit ed States in terms of probable volumes that can be marketed and competitive prices that can be realized. * Examine potential chemical plant locations in order to minimize barite ore, raw materials and final product transportation costs. * Examine the potential market for by-product sodium sulphide. 70 Barite and Fluorspar in Ontario Selected Bibliography Selected Bibliography Resources Andrews, P.R.A. and Ceilings, R.K. 1990. Barytes in Canada; Industrial Minerals, January, 1990, p.46-57. Barnes, L.H. 1979. Geochemistry of Hydrothermal Ore Deposits; second edition, Wiley Interscience Publication, John Wiley and Sons Inc., New York, p.471-490. Barron, K.H., Duke, N.A. and Hodder, R.W. 1989. Petrology of the Springpole Lake Alkalic Volcanic Complex; in Geoscience Research Grant Program, Summary of Research 1988-1989, Ontario Geological Survey, Miscellaneous Paper 143, p.133145. Bill, H. and Calas, G. 1978. Color Centers, Associated Rare-Earth Ions, and the Origin of Coloration in Natural Fluorites; Physics and Chemistry of Minerals, v.3, p. 117-131. Bright, E.G. 1983. Precambrian Geology of the Centre Lake Area, Western Part, Haliburton and Hastings Counties; Ontario Geological Survey, Map. P.2597, scale 1:15,840. Brown, R.L. 1973. Geological Report on Asarco Claims, Gravel Bay Fluorite Project, Township 87, Thunder Bay Mining Division, District of Thunder Bay; Ministry of Northern Development and Mines Assessment File No. 2.1361, Toronto. Burrows, A.G. 1981. The Matachewan Gold Area; Ontario Bureau of Mines, v.27, pt. l, p. 215-240. Carter M.W. 1987. Alkalic Rocks of the Thunder Bay Area; in Summary of Field Work and Other Activities 1987, Ontario Geological Survey, Miscellaneous Paper 137, p. 109-116. . 1989. Alkalic Rocks of the Thunder Bay Area; in Summary of Field Work and Other Activities 1989, Ontario Geological Survey, Miscellaneous Paper 146, p. 74-78. Carter, M.W., Mcilwaine, W.H. and Wisbey, P.A. 1971. NipigonSchreiber, Geological Compilation Series, Thunder Bay District, Map 2232, scale 1:253,440, revised after Pye, E.G. 1966, Map 2137. Deer, W.A., Howie, R.A., Zussman, J. 1980. An Introduction to the Rock-Forming Minerals; Longman Group Limited, London, 528 p. Dickson, T.B. and Trinder, I.D. 1989. Report on the 1989 Phase l Exploration Program, Fluorite-Barite Properties, Madoc and Huntingdon townships, Ontario, NTS 31C/5, C/6, C/l l, C/12, prepared for Harrington Sound Resources Incorporated by Derry, Michener, Booth, and Wahl, Ministry of Northern Development and Mines Assessment File 2.12688. Easton, R.M. 1989. Regional Patterns and Mineralization Associated with the Deloro Granite, Grenville Province, Madoc Area; Summary of Field Work and Other Activities 1989. Ontario Geological Survey, Miscellaneous Paper 146, p.158-168. Franklin, J.M. and Mitchell, R.H. 1977. Lead-Zinc-Barite Veins of the Dorion Area, Thunder Bay District, Ontario; Canadian Journal of Earth Sciences, v.14, No. 9, p.1963-1979. Friesen, B., Kusins, B., Kennedy, P. and Brown, P. 1985. Geology of the Golden Giant; Canadian Mining Journal, July 1985, p.53-54. Geul, J.J.C. 1973. Geology of Crooks Township, Jarvis and Prince Locations and Offshore Islands, District of Thunder Bay; Ontario Department of Mines, Geological Report 10Z, 43p. Giiddon, D.J. 1985. The Mineralogy and Genesis of the Archean Hemlo Barite Occurrences in Northern Ontario; unpublished MSc. thesis, Lakehead University, Thunder Bay, Ontario, 110 p. Guillet, G.R. 1963. Barite in Ontario; Ontario Department of Mines, Industrial Mineral Report Number 10, 42p. . 1964. Fluorspar in Ontario; Ontario Department of Mines, Industrial Mineral Report Number 12, 68p. 71 Harris, D.C. 1986. The Hemlo Gold Deposits, Ontario; Geological Association of Canada - Mineralogical Association of Canada - Canadian Geophysical Union Joint Annual Meeting 1986, Ottawa, Ontario, Field Trip 4: Guidebook, 74p. . 1989. The Mineralogy and Geochemistry of the Hemlo Gold Deposits, Ontario; Geological Survey of Canada, Economic Geology Report 38, 88p. Hewitt, D.F. 1968. Geology of Madoc Township and the North Part of Huntingdon Township, Hastings County; Ontario Department of Mines, Geological Report 73, 45p. Huhon, H. 1986. The Hemlo Gold Deposit, Ontario, Canada: A central portion of a large scale, wide zone of heterogeneous ductile shear; in Macdonald, A.J. ed., Proceedings of Gold '86, an Internation Symposium of the Geology of Gold; Toronto,1986, p.379-387. Junnila, R.M. 1989. 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Letter to Landair Explorations Limited; Ministry of Northern Development and Mines Assessment Files, Tweed. Melanson, F., and Robinson, G. 1982. The Fluorite Mines of Madoc, Ontario; Mineralogical Record, v.13, p.87-92. Mielke, R. 1977. Boulangerite and Associated Minerals of the Rogers Mine, Madoc, Ontario; unpublished BSc. thesis, University of Waterloo, Waterloo, Ontario, 57p. Miller, R. 1981. Petrology of Nepheline-Bearing Rocks in Glamorgan and Monmouth Townships, Ontario; unpublished MSc. thesis, University of Toronto, Toronto, Ontario, 376p. Muir, T.L. 1982. Geology of the Heron Bay Area, District of Thunder Bay; Ontario Geological Survey, Report 218, 89p. . 1983. Geology of the Hemlo-Heron Bay Area; in Geology of Gold in Ontario, ed. A.C. Colvine, Ontario Geological Survey, Miscellaneous Paper 110, p.230-239. Naldrett, D.L., LaChaine, A., and Naldrett, S.N. 1987. Rare Earth Elements, Thermal History, and the Color of Natural Fluorites; Canadian Journal of Earth Sciences, v.24, p.2082-2088. Patterson, G.C. 1984. Field Trip Guidebook to the Hemlo Area; Ontario Geological Survey, Miscellaneous Paper 118, 32p. Pye, E.G. and Fenwick, K.G. 1963. Atikokan-Lakehead Sheet. Geological Compilation Series, Kenora, Rainy River, and Thunder Bay Districts, Map 2065, scale 1:253,440. Roach, D. 1987. Barite Bodies West of Hemlo, Ontario, Petrofab ric and Geochemical Study; unpublished MSc. thesis, University of Ottawa, Ottawa, Ontario, 136p. Rupert, R.J. 1963. A Study of the Fluorspar Mines near Madoc, Ontario; unpublished BSc. thesis, Queen's University, Kingston, Ontario, 26p. Sabina, A.P. 1963. Rocks and Minerals for the Collector, Sudbury to Winnipeg; Geological Survey of Canada Paper 63-18, 69p. 72 . 1971. Rocks and Minerals for the Collector, Ottawa to North Bay, Ontario; Hull to Waltham, Quebec; Geological Survey of Canada, Paper 70-50, 130p. . 1974. Rocks and Minerals for the Collector, CobaltBelleterre-Timmins; Ontario and Quebec; Geological Survey of Canada, Paper 73-13 199p. . 1983. Rocks and Minerals for the Collector, Kingston, Ontario, to Lac St. Jean, Quebec; Geological Survey of Canada, Miscellaneous Report 32, 130p. . 1986. Rocks and Minerals for the Collector, BancroftParry Sound Area and Southern Ontario; Geological Survey of Canada, Miscellaneous Report 39, 182p. . 1987. Rocks and Minerals for the Collector, HullManiwaki, Quebec, Ottawa-Peterborough, Ontario; Geological Survey of Canada, Miscellaneous Report 41, 141p. Sage, R.P. and Breaks, F.W. 1982. Geology of the Cat LakePickle Lake Area; Ontario Geological Survey, Report 207, 238p. Satterly, J. 1956. Radioactive Mineral Occurrences in the Bancroft Area; Ontario Department of Mines, v.65 pt. 6, p.l176. . 1970. Aeromagnetic Maps of Carbonatite-Alkalic Complexes in Ontario, Ontario Department of Mines, Map P. 452 (revised), scale 1:4,245,120. Sinclair, W. 1982. 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Geological and Geophysical Studies of the Madoc Fluorite Area, Southern Ontario; in Summary of Field Work and Other Activities 1987, Ontario Geological Survey, Miscellaneous Paper 137, p.316323. . 1988. Structural Geology of the Madoc Fluorite Area, Southern Ontario; in Summary of Field Work and Other Activities 1988, Ontario Geological Survey, Miscellaneous Paper 141, p.363-367. -. 1989. Exploration Targets in the Madoc Fluorite Area, Southern Ontario; Summary of Field Work and Other Activities 1989, Ontario Geological Survey, Miscellaneous Paper 146, p. 180-185. Trowell, N.F. 1983. Geology of the Sturgeon Lake Area, Districts of Thunder Bay and Kenora; Ontario Geological Survey, Report 221, p.l-97. Valliant, R.I. and Bradbrook, C.J. 1986. Relationship between Stratigraphy, Faults, and Gold Deposits, Page-Williams Mine, Hemlo, Ontario, Canada; in Macdonald, A.E., ed., Proceedings of Gold '86, an International Symposium of the Geology of Gold, Toronto 1986, p.355-361. Vos, M.A., Abolins, T., and Smith, V. 1982. Industrial Minerals of Northern Ontario, Supplement 1; Ontario Geological Survey, Open File Report 5388, 344p. Vos, M.A., Abolins, T., McKnight, R.L.W., and Smith, V. 1983. Industrial Minerals of Northern Ontario, Part 1; Ontario Geological Survey, Open File Report 5386, 709p. Barite and Fluorspar in Ontario Walford, P., Stephens, J., Skrecky, G. and Barnett, R. 1986. The Geology of the "A" zone, Page Williams Mine, Hemlo, Ontario, Canada; in Macdonald, A.J., ed., Proceedings of Gold '86, an International Symposium of the Geology of Gold; Toronto 1986, p.362-378. Williams, D.A., and Thompson, L.G.D. 1986. Structural Setting of the Fluorite Vein Deposits of the Madoc Area, Southern Ontario; in Summary of Field Work and Other Activities 1986, Ontario Geological Survey, Miscellaneous Paper 132, p.347350. Wilson, M.E. 1929. Fluorspar Deposits of Canada; Canada Department of Mines, Geological Survey, Economic Geology Series Number 6, 97p. Woolley, A.R. 1987. Alkaline Rocks and Carbonatites of the World, Part l, North and South America, British Museum, London, England, p. l-71. Wu, T. 1984. Geochemistry and Petrogenesis of Some Granitoids in the Grenville Province of Ontario and their Tectonic Implications; unpublished PhD. thesis, University of Western Ontario, London, Ontario, 623p. Options for Production Andrews, P.R.A. and Collings, R.K. 1990. Barytes in Canada; Industrial Minerals, No. 268, January 1990, p.46-57. Collings, R.K. and Andrews, P.R.A. 1988a. Summary Report No. 1: Barite: CANMET Report 88-2E, January 1988, 38p. . 1988b. Summary Report No.3: Fluorite; CANMET Report 88-4E, January 1988, 30p. Faith, W., Lowenheim, F. and Moran, M. 1975. Industrial Chemicals, 4th Ed., Wiley Interscience, New York, p.121-125. Griffiths, J.B., Ed. 1988. Raw Materials for Pigments, Fillers and Extenders, Industrial Minerals, Consumer Survey, p. 146-153. Guillet, G.R. and Kriens, J. 1984. Ontario and the Mineral Filler Industry; Ontario Ministry of Natural Resources, Industrial Mineral Background Paper No. 5, p. 15-28. Kirk, R.E., Othmer, D.F., Grayson, M. and Eckroth, D. 1984. Encyclopedia of Chemical Technology, Wiley Interscience, 3rd ed., v.3, p.463-479. Law, Sigurdson b Associates and SRI International 1989. Inorganic Chemicals - Prospects for Ontario's Industrial Minerals; Ontario Ministry of Northern Development and Mines, Industrial Mineral Background Paper 11, 93p. McKetta, J.J. and Cunningham, W.A. 1976. Encyclopedia of Chemical Processing and Design, M. Dekker, U.S.A.; vol. 23, p.270-295 (Fluorspar); v.4, p.50-65 (Barium Compounds). Prud'homme, M. 1989. The Market for Acid Grade Fluorspar in North America; CIM Directory, vol. 23 1989, p.133-138. Sittig, M. 1968. Inorganic Chemicals and Metallurgical Process Encyclopedia; Noyes Data Corp., U.S.A., p.93-94. Ullman, F. and Gerhatz, W. eds, 1985. Encyclopedia of Industrial Chemistry, 5th Ed., VCH Publishers, U.S.A., v.A3, p.325-341. White, E.D. 1949. The Plant that Barite Built, in Chemical Engineering, April 1949, p.91-95, p.128-131. Selected Bibliography 73 74 Barite and Fluorspar in Ontario Appendix A Barite Mill Processing Equipment Major Items and Typical Costs (not installed) 1.Barite Mill, 30,000 tonnes per year Thunder Bay-Matachewan EQUIPMENT NAME SIZE TYPICAL COST S Jaw Crusher 24" x 36" 100,000 Hammer Mill 10" x 20" 50,000 Jig Duplex 24" x 36" 20,000 Shaking Table Full Size 16,000 Rod Mill, 100 HP 5'Dia. x 10' * 70,000 Flotation Cells 6 @ 1.4 m 360,000 Vacuum Filter c/w Pumps 6' Dia. x 4 Disc * 50,000 Rotary Dryer c/w Fuel System 6' Dia. x 36' *250,000 Building 12 m x 24 m 60,000 'Denotes used equipment price. Appendix A 75 Appendix A Barite Mill Processing Equipment Major Items and Typical Costs (not installed) 2.Barite Mill, 30,000 tonnes per year, Hemlo Gold Mill Tailings EQUIPMENT NAME SIZE TYPICAL COST Flotation Cells (Pyrite) 6 @ 5 m 3150,000 Flotation Cells (Molybdenum) 6 @ 5 m 18 @ 1.4 m3 3150,000 270,000 Flotation Cells (Barite) 6 @ 3 m 18 @ 0.7 m3 3120,000 126,000 Vacuum Filter c/w Pumps 6' Dia. x 4 Disc * 50,000 Rotary Dryer c/w Fuel System 6' Dia. x 36' * 250,000 Building 18 m x 43 m 170,000 'Denotes used equipment price. 76 Barite and Fluorspar in Ontario Appendix B Barium Chemicals Plant Equipment Major Items and Typical Costs (not installed) 1.Barium Sulphide Plant EQUIPMENT NAME SIZE/CAPACITY TYPICAL COST Barite Mill 5.0 t/h, -1/2" to - 20 mesh Rotary Kiln c/w Fuel System'1, 250 0 C, A Pollution Control 6' Dia. x 60', Refractory Lined Sulphide Grinder 3.2 t/h, Clinker to -20 mesh Barite Silos (2) 12' Dia. x 32' 40,000 ea Coal Silo 12' Dia. x 32' 40,000 Barite Feeder 4.0 t/h 40,000 Coal Feeder 0.5 t/h 20,000 BaS Solution Tanks (4) c/w Agitators 8' Dia. x 14', SS 36,000 ea Decant Tank 10' Dia. x 9', SS 24,000 BaS Storage Tanks (2) c/w Agitators 12' Dia. x 20', SS BaS Sludge Tank c/w Agitator 8' Dia. x 14', SS BaS Screen 3' Dia. Single Deck Appendix B 100,000 1,400,000 40,000 40,000 ea 36,000 8,000 77 Appendix B Barium Chemicals Plant Equipment Major Items and Typical Costs (not installed) 2. Barium Carbonate C+ Sulphate) Plant EQUIPMENT NAME SIZE/CAPACITY TYPICAL COST S BaCOs Reaction Tank c/w Agitator 8' Dia. x 14', SS Vacuum Filters (2) c/w Pumps 6' Dia. x 6', SS BaCOa Paddle Dryer 450 sq ft heat transfer area, SS BaCOa Grinder 2.5 t/h, -1/16" to -10um Na2S Evap/Crystallizer 10,000 kg/h evap, SS 400,000 Na2S Centrifuge 4 mS/h feed, 30 0Xo solids, SS 100,000 Na2S Paddle Dryer 90 sq ft area, SS 120,000 Na2C03 Silos (2) 12' Dia. x 32' Na2COs Solution Tank c/w Agitator 8' Dia. x 8', SS 24,000 BaS Solution Tank c/w Agitator 12' Dia. x 14', SS 36,000 BaCOs Screen 3' Dia. Single Deck 8,000 Na2S Screen 2'6" Dia. Single Deck 6,000 BaCO3 Silos (2) 12' Dia. x 24' 35,000 ea Na2S Silos (2) 12' Dia. x 32' 40,000 ea Na2SO4 Solution Tank 8' Dia. x 8', SS 24,000 BaSO4 Silo 8' Dia. x 14' 20,000 78 36,000 60,000 ea 320,000 32,000 40,000 ea Barite and Fluorspar in Ontario Appendix B Barium Chemicals Plant Equipment Major Items and Typical Costs (not installed) 3. Barium Chloride Plant EQUIPMENT NAME SIZE/CAPACITY BaCl2 Reaction Tank c/w Agitator 6' Dia. x 6', Lined BaCI 2 Solution Filters (2) 10 USgpm cont. Alloy 20 BaCl2 Evap/Cryst 1 .200 kg/h evap, Host alloy/Titanium BaCla Vacuum Filter 3' Dia. x 4', Alloy 20 BaCl2 Paddle Dryer 90 sq ft area, Alloy 20 Na2S Reaction Tank 6' Dia. x 6', SS HCI Storage Tanks (2) 12' Dia. x 16', Lined NaOH Storage Tank 14' Dia. x 18' BaCl2 Screen 2' Dia. Single Deck BaCI 2 Silo 10' Dia x 20' Appendix B TYPICAL COST S 40,000 15,000 ea 270,000 30,000 150,000 15,000 38,000 ea 45,000 5,000 30,000 79 Appendix B Barium Chemicals Plant Equipment Major Items and Typical Costs (not installed) 4. Barium Oxide/Hydroxide Plant EQUIPMENT NAME SIZE/CAPACITY TYPICAL COST S BaCOa Feeder 0.5 t/h BaO Fluid Bed Reactor c/w Fuel System, Cyclone 5' Dia. x 20', SS 300,000 BaO Paddle Cooler 65 sq ft area, SS 100,000 BaO Grinder 0.4 t/h, -1/8" to -10um 20,000 BaO Feeder 0.3 t/h 18,000 Ba(OH)2 Reaction 35 ftS/h Mixer, VesseISS Ba(OH) 2 Drum Cooler A Flaker 0.5 t/h 40,000 Ba(OH) 2 Dryer 4' Dia. x 20', SS 80,000 Ba(OH)2 Screen 2' Dia. Single Deck BaO Silo 8' Dia. x 18' Ba(OH)2 Silos (2) 10' Dia. x 20' 80 20,000 120,000 5,000 24,000 30,000 ea Barite and Fluorspar in Ontario Appendix C Fluorspar Mill Processing Equipment Major Items and Typical Costs (not installed) EQUIPMENT NAME SIZE TYPICAL COST S Jaw Crusher 24" x 36" 100,000 Hammer Mill 1 0" x 20" 50,000 Jig Duplex 24" x 36" 20,000 Shaking Table Full Size 16,000 Rod Mill, 100 HP 5' x 10' Flotation Cells 18 @ 1.4 m 3 180,000 Flotation Cells 30 @ 0.7 m 3 210,000 Vacuum Filter 6' Dia. x 4 Disc. * 50,000 Rotary Dryer 6' Dia. x 36' * 250,000 Building 12 m x 30 m 70,000 * * 70,000 Denotes used equipment price. Appendix C 81
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